[geo] Re: Comments on Irvine et al. (2019) by Alan Robock

2019-03-13 Thread David Keith


Alan

 

Thanks for taking the time to write this. Responses below. Look forward to 
discussing in person, best over a beer. 


(N.B., i don't get emails from this-just too much inbox--so pls anyone feel 
free to email me directly with posts...)

 

Yours,

David


 First of all, I want to make clear that I completely agree with David 
Keith that mitigation is the solution to the global warming problem and we 
have to work urgently to switch our energy system away from fossil fuels, 
that we need much more research on solar geoengineering, and that we should 
not ever do solar geoengineering until we have a much better understanding 
of the risks it might pose as compared to the risks of not doing it.  

 

I suspect you agree, but nevertheless I need to say it: Mitigation is 
necessary, but mitigation is *not* “the solution”. Cutting emissions to 
zero stops putting CO2 in the air. The CO2 and climate risk are still 
there. We need adaptation. But adaption is not *the solution*. Neither is 
solar geo. Neither is carbon removal. Complex problems like climate rarely 
have a single solution. The overarching question here is should solar geo 
be part of the solution? My answer is I don’t know. But there is enough 
reason to think it should be that I think serious research makes sense. 

But I disagree with his framing of this new paper.  In his March 11 
tweet he said, “New paper with Kerry Emanuel and a GFDL team in 
@NatureClimate, using high-resolution model to test which regions would be 
made worse off by solar geoengineering--find that no region is made worse 
off in any of the major climate impact indicators we examined.”  He fails 
to mention that many places on Earth might be worse off if we follow their 
scenario if we consider more than just temperature and precipitation minus 
evaporation.  In any case, “worse” as compared to what?  If we rapidly 
begin mitigation now, that is rapidly reduce our CO2 emissions to zero by 
switching our power to wind and solar, we will be much better off than a 
business-as-usual future, or one with geoengineering.  I don’t think it is 
useful or correct to imply that geoengineering is a good or safe idea.

Guilty as charged. The tweet is too simple. But I think it’s clear from my 
work and many other tweets in about this paper that I and other authors 
(see Kerry’s interview 
<https://www.wbur.org/radioboston/2019/03/11/aerosols-global-warming>) know 
there will--of cours--be impacts of any solar geo method. There is *no *way 
geo can be risk free. 

 

Quibble: It’s not fair for you to say “just temperature and precipitation 
minus evaporation”, as you now we did look at more than T and P-E, we did 
Tmax, Pmax, P,and some look at seasonal, and Tropical Cyclone intensity. 
But, quibble aside – there is lots more to do. For example, it would be 
nice to do a long multi-century run and look at droughts. 

 

More important. You assert “If we rapidly begin mitigation now, that is 
rapidly reduce our CO2 emissions to zero by switching our power to wind and 
solar, we will be much better off than a business-as-usual future, or one 
with geoengineering.” I don’t think this is supported by data. There is *no 
doubt* that mitigation is far better than BAU. But it’s quite possible that 
mitigation plus some solar geo is less risky than mitigation alone. Or, 
maybe not. But I don’t know. And I don’t know how you can be sure. This is 
the essence of the debate. 


Irvine et al. (2019) utilized a high-resolution climate model from GFDL 
to do some stratospheric geoengineering experiments, but the results they 
got must be considered in the context of the limitations of the work.  
Because they mimicked stratospheric geoengineering by turning down the 
solar constant rather than modeling stratospheric aerosols, they ignored a 
large number of potential impacts, including more diffuse radiation, 
heating of the stratosphere, and impacts on stratospheric ozone.  These 
latter two factors would change atmospheric circulation as well as affect 
the potential intensity of tropical cyclones.  And the changes in 
circulation will change the temperature and precipitation patterns that 
result.

It also must be kept in mind that they considered only one particular 
scenario of stratospheric geoengineering.  And there is no way to do what 
they modeled, as we cannot turn down the Sun.  The technology to create an 
aerosol cloud in the stratosphere does not currently exist.  Various 
designs have been described that would cost $50,000,000,000 to 
$200,000,000,000 (50-200 billion dollars) per year to implement, and which 
would result in significant increases in acid rain as well as a host of 
other possible risks.  (This calculation came from the estimates of Robock 
et al. (2009), McClellan et al. (2010, 2012), Smith and Wagner (2018), and 
deVries et al. (2018) of how much it would cost to construct and operate 
planes to deliver enough SO2 or H2SO4 to the strato

[geo] Re: Cheap Carbon Capture

2018-06-16 Thread David Keith


I don’t normally monitor this group but someone suggest that respond to 
this comment so here goes…

 

1. Di Marco is entirely correct that we can’t make fuels that are precisely 
carbon neutral with the gas-fired system. Our estimate is that fuels made 
using that system would have WTW carbon intensities of roughly 30 gCO2/MJ. 
This is still better than most biofuels and about three times better than 
typical fossils but it’s not zero. David Robert’s Vox article got this 
right. 


2. As we hint in the paper we are developing all-electric options for the 
fuels production. 


3. I agree that fossil prices will fall, under life-cycle standard regs 
like LCFS our competition is not directly fossils but rather other options: 
H2, NH3, and batteries. We think air-to-fuels does very well against that 
competition as a long-term pathway to power heavy transportation. 


-David

On Friday, 15 June 2018 17:03:40 UTC-4, Leon Di Marco wrote:
>
>
>
> *Perhaps my last post was rather too hard on Christopher Preston, who is 
> not an expertHere is an illustration of the dubious nature of some of the 
> claims that have been made, using the attached paper just published in 
> Joule by Keith et al , entitled  A Process for Capturing CO2 from the 
> Atmosphere, which has been the subject of some publicity.  U**nder the 
> heading Context and Scale, ** the paper gives this description -  *
> *"An industrial process for large-scale capture of atmospheric CO2 (DAC) 
> serves two roles. First, as a source of CO2 for making carbon-neutral 
> hydrocarbon fuels,"*
>
> *The cover page shows an infographic  illustrating  1 tCO2 being captured 
> by a DAC machine, producing a 1.3-1.5 t stream  of CO2 intended for "Fuels 
> or Sequestration" .  The source of the additional CO2 is explained **in 
> the body of the paper at page 2-*
> *"*
> *At full capacity, this plant captures 0.98 Mt-CO2/year from *
> *the atmosphere and delivers a *
> *1.46 Mt-CO2/year stream of dry CO2 at 15 MPa. The additional 0.48 
> Mt-CO2/year is produced by on-site combustion of natural gas to meet all 
> plant thermal and electrical requirements."*
>
> *If the product from this machine is intended to be fuel,  1/3 of the CO2 
> output comes from burning natural gas, and thus the fuel cannot be carbon 
> neutral.   Alternatively, if the CO2 is buried in sites intended for 
> enhanced oil recovery, then there will be an additional carbon footprint.  
>A combination of both (by burying 1/3 of the CO2) will still have 
> consequences for the carbon footprint of the fuel.*
>
> * The main message from the paper is the formal refutation of the results 
> from the report on the cost of DAC produced by the APS in 2011. But that 
> message has long been overtaken by the findings from several commercial 
> players who have been working on DAC .   Beyond that its message is 
> controversial and smacks of commercial hype.  *
>
> *It is possible to produce carbon negative power using a plant using 
> natural gas, and even carbon negative synthetic liquid fuels ( if that is 
> what is required) but the likelyhood is that low cost carbon offsets from 
> DAC will be used to cancel the emissions created by burning fossil fuels. 
> The cost of oil will fall as demand reduces and that will make it difficult 
> for synthetic fuels to survive.*
>
>
>
>
>
>
> On Thursday, June 14, 2018 at 10:10:54 PM UTC+1, Christopher Preston wrote:
>>
>> A few thoughts on last week's good news about the potential for much 
>> cheaper DAC.
>>
>>
>> https://plastocene.com/2018/06/14/catching-carbon-why-cheap-still-comes-with-a-cost
>>
>

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[geo] Re: [CDR] The International Conference on Negative CO2 Emissions » 22-24 May 2018

2017-11-24 Thread David Keith


Peter

I’m sorry you’re frustrated. I don’t think your interpretation is entirely 
fair.


It would be ridiculous to claim that solar geoengineering is “necessary”.


I did not make that claim here and I believe I’ve been consistent on this 
over years in writing and speaking. I don’t believe I said anything to 
contradict that view in this interview. It’s true I did not specifically 
say in this interview that this was not true. But note that this interview 
this was tightly edited and omitted many things I often say about 
governance and about context including mitigation and carbon removal. For a 
longer unedited video that does mention carbon removal see: 
https://www.technologyreview.com/video/609398/the-growing-case-for-geoengineering/


I have been clear consistently that solar geoengineering has substantial 
risks, that it is, at best, a partial supplement to emissions reductions.

Here’s how I see the trade-off between emissions reductions, carbon 
removal, and solar geoengineering.


Emissions reductions are necessary if we want a stable climate. If we try 
to continue emissions and offset them with increasing solar geoengineering 
the world will walk further and further away from the current climate with 
higher and higher risks. One could, in principle get a stable climate, by 
continuing emissions and offsetting them with carbon removal. But I fail to 
see why it would make economic or environmental sense to have massive 
carbon removal (with its attendant costs and environmental impacts) while 
we still have massive emissions. If there is truly a low impact way to do 
carbon removal that is significantly cheaper than emissions reductions, 
then I would change my view on this. (Yes, I know you believe you can do 
carbon removal at some low number like 30 or $50 a ton. I truly hope you’re 
correct. I simply haven’t seen the evidence yet.)


While emissions are high I don’t believe there is a meaningful distinction 
between emissions mitigation and carbon removal. The climate can’t tell the 
difference between a ton not emitted in a ton emitted and recaptured. So, 
while emissions are high, I think we should only put significant effort 
into large-scale deployment of carbon removal if it is cheaper than other 
methods of reducing emissions, or if it has lower environmental impacts and 
roughly the same cost.


Once emissions get down towards zero carbon removal provides a unique 
ability to reduce concentrations. Once emissions get to zero carbon removal 
can do something that can’t be done by emissions mitigation or solar 
geoengineering. That’s part of the reason I’m very proud to have worked on 
carbon removal from my early work on BECCS (early papers, first PhD of the 
topic) to my work at Carbon Engineering). I would therefore like to see 
serious effort to developing carbon removal even if it is not now cheaper 
or otherwise better than emissions reduction. And serious development will 
entail limited deployment. It makes sense to do this during the time 
emissions are high to buy the option for net negative emissions once 
emissions get towards zero. 


Finally, solar geoengineering may provide a way to substantially reduce 
climate risks during a carbon concentration peak. A peak defined by 
continued positive emissions on the front and by carbon removal on the far 
side.


Finally, note that, contrary to your assertion, solar geoengineering does 
in fact provide some significant reduction in carbon concentrations 
.
 


 

Peter, I think were roughly on the same side. 

I think the work you’re doing is terrific.

 

Yours,
David


N.B., I am not subscribed to this list so please email me or post on 
twitter if you want to continue the conversation. 



On Sunday, 19 November 2017 11:34:14 UTC-5, Peter Eisenberger wrote:
>
> David Keith was on TV and did what I have expressed concern about 
> generally about the advocacy for SRM
> He accepted the framework that we will fail to address the carbon 
> emissions reduction targets , failed to mention the CDR 
> option he himself helped pioneer and then pushed off concerns expressed 
> about doing SRM by saying doing nothing 
> also has risks ( not even mentioning that acidification of the ocean will 
> continue for sure and the continuing buildup of co2 etc )  . But most 
> importantly he supported the choice as being between doing nothing or doing 
> SRM which as a previous comment pointed out will be embraced by those who 
> want to do nothing that doing this will enable us to avoid the adverse 
> impacts of climate change and thus is acceptable as a response to climate 
> change threat 
>
> My general point has been and continues to be that if us scientists allow 
> our advocacy for a particular approach to determine what we say and not 
> discipline ourselves with
> a overall coherent approach we will become (are) part of the problem and 
> not part of the solution 
>

[geo] Postdocs in solar geoengineering

2016-01-04 Thread David Keith


Please forgive the mass mailing. I am looking to recruit couple of postdocs 
to work on solar geoengineering. I am particularly interested in people 
with a background in atmospheric science and chemistry, but also interested 
in an applicant from the social sciences. 

 

For star quality applicants, the Harvard Environmental Fellows Program 
<http://environment.harvard.edu/environmental-fellows-program> gives 
fellows, independence, good pay, and access to a broad set of faculty 
across campus. It’s deadline is 13th January (next Wednesday). If you know 
anyone who might be interested and suitable please point them my way ASAP. (
http://environment.harvard.edu/environmental-fellows-program). 

 

N.B., As Alan announced, in a small step to professionalizing work in this 
field several colleagues and I got a Gordon Conference on Solar 
Geoengineering approved, with the first meeting to be held in 2017.

 

Happy New Year,

David


 

*David Keith*

Gordon McKay Professor of Applied Physics, 

   School of Engineering and Applied Sciences (SEAS); and,

Professor of Public Policy,

   Kennedy School of Government,

Harvard University

 

david_ke...@harvard.edu

www.keith.seas.harvard.edu@DKeithClimate

 

Executive Chairman, Carbon Engineering

www.carbonengineering.com

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[geo] 2 new papers: solid aerosols and liablity

2015-04-29 Thread David Keith
Here two new papers that may be of interest to the group.

Debra K. Weisenstein and David W. Keith. (2015).  Solar geoengineering using 
solid aerosol in the stratosphere. Atmospheric Chemistry and Physics Discuss., 
15: 11799-1185. www.atmos-chem-phys-discuss.net/15/11799/2015/
There been a whole sequence of papers examining the possibility of solid 
aerosols for solar geoengineering the stratosphere, but none have look 
seriously at the fact that solid aerosols will interact with each other and 
with the background sulfate. We show that, for a given amount of radiative 
forcing, solid aerosols *might* be able to reduce some environmental risks: 
ozone, diffuse light, and heating of the lower stratosphere. I showed figures 
from the work in my longnow talk: 
http://longnow.org/seminars/02015/feb/17/patient-geoengineering/


Joshua B. Horton, Andrew Parker, and David Keith. (2015). Liability for Solar 
Geoengineering: Historical Precedents, Contemporary Innovations, and Governance 
Possibilities. NYU Environmental Law Journal, 22: 225-273.
The absence of liability regimes is sometimes assumed to be a showstopper for 
solar geoengineering. We examine a set of international liability regimes 
mostly associated with environmental risks, and suggest that there is a broad 
legal and historical precedent that might serve as a basis to develop a regime 
for solar geoengineering.

Papers are here: http://www.keith.seas.harvard.edu/srm-papers/

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[geo] 2 new papers: solid aerosols and liablity

2015-04-29 Thread David Keith
Here two new papers that may be of interest to the group.

Debra K. Weisenstein and David W. Keith. (2015).  Solar geoengineering using 
solid aerosol in the stratosphere. Atmospheric Chemistry and Physics Discuss., 
15: 11799-1185. www.atmos-chem-phys-discuss.net/15/11799/2015/
There been a whole sequence of papers examining the possibility of solid 
aerosols for solar geoengineering the stratosphere, but none have look 
seriously at the fact that solid aerosols will interact with each other and 
with the background sulfate. We show that, for a given amount of radiative 
forcing, solid aerosols *might* be able to reduce some environmental risks: 
ozone, diffuse light, and heating of the lower stratosphere. I showed figures 
from the work in my longnow talk: 
http://longnow.org/seminars/02015/feb/17/patient-geoengineering/


Joshua B. Horton, Andrew Parker, and David Keith. (2015). Liability for Solar 
Geoengineering: Historical Precedents, Contemporary Innovations, and Governance 
Possibilities. NYU Environmental Law Journal, 22: 225-273.
The absence of liability regimes is sometimes assumed to be a showstopper for 
solar geoengineering. We examine a set of international liability regimes 
mostly associated with environmental risks, and suggest that there is a broad 
legal and historical precedent that might serve as a basis to develop a regime 
for solar geoengineering.

Papers are here: http://www.keith.seas.harvard.edu/srm-papers/

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[geo] Self promo: Temporary, moderate, and responsive == patient

2015-03-13 Thread David Keith


Here's a new(ish) paper and related talk:

 

David W. Keith and Douglas G. MacMartin. (2015) A temporary, moderate and 
responsive scenario for solar geoengineering 
http://keith.seas.harvard.edu/papers/174.Keith.MacMartin.ATemporaryModerateandResponsiveScenarioforSolarGeoengineering.pdf
. Nature Climate Change, DOI: 10.1038/NCLIMATE2493. The paper is available 
through 
the link above. 

 

Here's video of a talk I gave at Long Now foundation. Stewart Brand gave me 
the title, Patient Geoengineering. This talk includes longer, more visual 
version of the argument in the paper mentioned above.

 http://longnow.org/seminars/02015/feb/17/patient-geoengineering/ 


David

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[geo] Opporties @ Harvard

2014-12-11 Thread David Keith
I am growing my research group at Harvard. Here are a few opportunities 
that might interest people on this list: 

Opportunities 
1. The Harvard Center for the Environment has a great fellowship program 
http://environment.harvard.edu/environmental-fellows-program for 
post-docs. It’s a high-profile competitive program that gives recipients 
lots of freedom and a good community. 
2. I will be taking at least one fellow through the Science Technology and 
Public Policy 
http://belfercenter.ksg.harvard.edu/project/44/science_technology_and_public_policy.html?page_id=348
 
program at the Belfer Center 
http://belfercenter.ksg.harvard.edu/index.html at the Kennedy School. 
These fellowships generally for post-docs, but they can be awarded to 
people without doctorates who have strong track-records in public policy 
work. 
3. I also hire post-docs directly. However I get lots of inquiries and 
generally only pay attention if I get recommendations from someone I know. 
4. Finally, there is a new Kennedy School fellowship for junior faculty or 
unusually qualified post-docs, the Louis Bacon Environmental Academic 
Fellow program. It provides full funding for one year’s residence at the 
Kennedys school. Let me know if you are interested. 


I am also funding researchers who want to visit for a few weeks. We expect 
to host an overlapping set of visitors working on solar geoengineering in 
May-June 2015. 


David 

 

David Keith

Gordon McKay Professor of Applied Physics, 

   School of Engineering and Applied Sciences (SEAS); and,

Professor of Public Policy,

   Kennedy School of Government,

Harvard University

david_ke...@harvard.edu

www.keith.seas.harvard.edu

 

 

 

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RE: [geo] Your Vector diagram

2012-11-30 Thread David Keith
Andrew

A few comments in response to this and the subsequent comment by

1. This vector representation is useful way to think about trade-offs when the 
climate response to CO2 and SRM is reasonably linear. This stuff is published 
as: Juan Moreno-Cruz, Katharine Ricke and David W. Keith. (2011). A simple 
model to account for regional inequalities in the effectiveness of solar 
radiation management. Climatic Change, doi: 10.1007/s10584-011-0103-z. 
(PDF)http://www.keith.seas.harvard.edu/papers/131.Moreno-Cruz.Inequality.SRM.e.pdf.
 Despite the hype about nonlinearity, models are quite linear in the region of 
interest, see the appendix to the paper.

2. I was surprised by our results. I expected the trade-offs to be much 
stronger. Doing this work pushed me to realize that SRM can do a substantially 
better job of compensating CO2-driven climate change than I had expected. (Of 
course, it does nothing about the geochemical impacts of CO2 such as ocean 
acidification.)

3. Yes, you can consider quantities other than temperature and precip; and 
quantities like soil moisture are certainly important.

4. Stephen Salter imply that these results were somehow particular to 
stratospheric sulfates, saying: I think that you must be referring to 
geo-engineering with stratospheric sulphur. With tropospheric salt you can vary 
precipitation in both directions by choosing the time and place to spray. This 
analysis is applicable to both. It is certainly true that if sea salt aerosol 
can be effectively used to alter cloud albedo over large areas--a proposition 
which is still quite uncertain--then it could be used to reduce (them 
eliminate) the trade-offs.

We looked at exactly this in a more recent paper examining how trade-offs can 
be reduced if you were able to adjust the intensity of SRM forcing at different 
locations in seasons:  Douglas G. MacMartin, David W. Keith, Ben Kravitz, and 
Ken Caldeira. (2012). Managing tradeoffs in geoengineering through optimal 
choice of non-uniform radiative forcing. Nature Climate Change, doi: 
10.1038/NCLIMATE1722. 
(PDFhttp://www.keith.seas.harvard.edu/preprints/158.MacMartin.etal.ManagingTradeoffsThroughNonRadForc.p.pdf).

Note that this paper explicitly looks at something people in this blog often 
ask about which is the ability to tune SRM to focus on restoring Arctic sea ice.

5. Finally, I do not understand your argument about soil moisture. Evaporation 
always equals precipitation the global mean. All else equal-- and it probably 
will not be--one expects variability to go down (not up) as you weaken the 
hydrological cycle. So my back of the envelope physics points the opposite way 
to yours. We look at this in one of the papers with Kate Ricke and found that 
at least the one case we looked at variability did go down.

Of course, model do not equal reality.

Yours,
David




From: geoengineering@googlegroups.com [mailto:geoengineering@googlegroups.com] 
On Behalf Of Andrew Lockley
Sent: Monday, November 26, 2012 7:08 AM
To: David Keith; geoengineering
Subject: [geo] Your Vector diagram


David

I remember the excellent vector diagram lecture you gave at Oxford.  In it you 
represented temperature and precipitation on a vector.diagram and showed that 
both cannot be simultaneously corrected exactly by geoengineering, but that the 
mismatch was small.

However, that would leave us in a world which was either slightly drier or 
slightly warmer than in a non-geoeng world - or a combination of both.

My concern is that things might be a bit more serious than that. If we consider 
a warmer world with the same level of precipitation, the surface evaporation 
world be higher and the relative atmospheric humidity would (I think) be lower. 
As a result, soil wetness may be very much lower, as  evapotranspiration would 
be higher. If rainfall patterns were perturbed, we might additionally get more 
variability in both wetness and precipitation.

So we could end up in a world with much drier soils, and possibly heavier 
storms, too.

Should your vectors therefore be soil wetness vs temperature, not precipitation 
vs temp?  Making a bad call on this could really hit agricultural outputs.

A
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RE: [geo] Cost analysis of stratospheric albedo modification delivery systems (ERL) Open Access

2012-09-05 Thread David Keith
Andrew



Answers to your questions about the our recent URL paper on stratospheric 
albedo modification delivery systems.



Q: Isn't this just a reformatted version of the Aurora flight report?

A: Essentially yes. The online supplemental information is the Aurora report, 
the paper is newly written but has relatively little view analysis. The paper 
puts the report in an archival peer-reviewed journal. We made minor 
improvements in response to review but nothing fundamental. We could have kept 
the report to ourselves until publication, but because our views about the 
importance of openness in this field we decide to release the entire report 
when it was completed following our internal peer-review.



Q: it ignores gas guns (which are half the price in $/kg of solid-propellant 
guns) and contradicts SPICE balloon cost estimates.  It works up aircraft way 
more than other tech, leading to unsurprisingly lower cost estimates of these 
technologies.  Coming up with low prices for worked up tech seems a common 
thread in papers.

A: This seems to me a very odd criticism of this paper. Unlike (to my 
knowledge) any other paper we examined all the different options in our scope 
using the same costing assumptions and industry-standard cost estimating 
relationships (CERs). I am not aware that the SPICE project has done anything 
similar.



We did not come into it with any particular bias towards airplanes and in 
practice we spent a lot of time on hybrid airships and on the balloon with hose 
option because analysis there was relatively harder to do. If you discount the 
section on existing aircraft which seems fair since there are no alternative 
options that are as ready to go, the section on new aircraft is not 
substantially longer than the sections on hybrid airships or the hose option.



Finally it seems like an odd criticism because in fact we found that the cost 
of hybrid airships, new aircraft, and the balloon with hose option were broadly 
comparable.



gas guns (which are half the price in $/kg of solid-propellant guns) We did not 
spend significant time on gas guns because we talked to David Whelan, US 
National Academy member and senior scientist at Boeing, one of the world 
experts on this topic, and he advised us that gas guns would not be a 
significant advantage for the altitude range that is relevant here. Even if gas 
guns were half the price of solid propellant guns as you assert, and I do not 
know of a study that shows that to be true when you count capital and operating 
costs, the cost would still be absurdly high compared to the other options 
investigated (hybrid airships, the balloon with hose, or regular aircraft) and 
therefore all but irrelevant.



David





-Original Message-
From: geoengineering@googlegroups.com [mailto:geoengineering@googlegroups.com] 
On Behalf Of Andrew Lockley
Sent: Thursday, August 30, 2012 5:52 PM
To: geoengineering; David Keith
Subject: [geo] Cost analysis of stratospheric albedo modification delivery 
systems (ERL) Open Access



Poster's note: Isn't this just a reformatted version of the Aurora flight 
report?  If so, it ignores gas guns (which are half the price in $/kg of 
solid-propellant guns) and contradicts SPICE balloon cost estimates.  It works 
up aircraft way more than other tech, leading to unsurprisingly lower cost 
estimates of these technologies.  Coming up with low prices for worked up tech 
seems a common thread in papers.

This could be clarified by authors generally, I feel.



http://iopscience.iop.org/1748-9326/7/3/034019



We perform engineering cost analyses of systems capable of delivering

1-5 million metric tonnes (Mt) of albedo modification material to altitudes of 
18-30 km. The goal is to compare a range of delivery systems evaluated on a 
consistent cost basis. Cost estimates are developed with statistical cost 
estimating relationships based on historical costs of aerospace development 
programs and operations concepts using labor rates appropriate to the 
operations. We evaluate existing aircraft cost of acquisition and operations, 
perform in-depth new aircraft and airship design studies and cost analyses, and 
survey rockets, guns, and suspended gas and slurry pipes, comparing their costs 
to those of aircraft and airships. Annual costs for delivery systems based on 
new aircraft designs are estimated to be $1-3B to deliver 1 Mt to 20-30 km or 
$2-8B to deliver 5 Mt to the same altitude range. Costs for hybrid airships may 
be competitive, but their large surface area complicates operations in high 
altitude wind shear, and development costs are more uncertain than those for 
airplanes. Pipes suspended by floating platforms provide low recurring costs to 
pump a liquid or gas to altitudes as high as  ~ 20 km, but the research, 
development, testing and evaluation costs of these systems are high and carry a 
large uncertainty; the pipe system's high operating pressures and tensile 
strength

RE: [geo] Cost analysis of stratospheric albedo modification delivery systems (ERL) Open Access

2012-09-05 Thread David Keith
Andrew

Our job was not to make an economic case [for or] against these technologies, 
it was just to do transparent evenhanded analysis.

On this topic I just don't have a bias about what the answer is. There are lots 
of weaknesses in the our study, but I think one of its strengths was that it 
used a relatively evenhanded treatment as none of the people involved has a 
particular attachment to or professional involvement in on any outcome. (I 
suppose you might argue that Aurora has primarily done aircraft, but Aurora now 
does contract engineering on a wide range of aerospace systems and I do not 
believe that strongly influence the outcome here. We are working on balloon 
systems with suspended tethers as part of our development of possible 
experiments). I think there are lots of very fine contributions in the work 
coming out of the SPICE group, but I do not think it is unfair to point out 
that this group is focused on developing a particular technology.

In any case, the big answer from this paper and several others are that costs 
of delivery are small enough that they don't matter in any sensible policy 
analysis. The goal of our paper was help establish that fact as well as to 
establish that delivery could be accomplished with technologies that could be 
procured from multiple vendors today.

It is fun to get into playing around with some particular technology to one 
loves to try and see if you can do the job a little bit cheaper. I have yet to 
see a coherent quantitative argument why it matters to get costs under the 
roughly few $/kg level we found here.

I would be happy to see a high quality analysis of a novel gun the system that 
showed that costs were substantially cheaper. But what is needed here is 
analysis not assertions. Saying that the Novim study notes the opportunity for 
substantial costs savings does not say much. As a contributor on the Novim 
study, I can tell you we spent far less time analyzing the gun system there and 
we did in the work Aurora.

David





-Original Message-
From: geoengineering@googlegroups.com [mailto:geoengineering@googlegroups.com] 
On Behalf Of Andrew Lockley
Sent: Wednesday, September 05, 2012 9:30 AM
To: David Keith
Cc: geoengineering
Subject: Re: [geo] Cost analysis of stratospheric albedo modification delivery 
systems (ERL) Open Access

David

Thanks for your reply.

For the avoidance of doubt, I was grouping airships and fixed-wing craft as 
'aircraft'.  I don't doubt that your work in this area was very valuable.  My 
concern is in the comparison of worked-up technology with less well developed 
technology.

For comparison, you can consider the recent Phil Trans A paper by the SPICE 
team, which considers similar issues.  This paper engineers the balloon system 
preferentially, and thus considers this to be a superior technology due to the 
cost improvements from this engineering process.  The tendency should be clear, 
but to state explicitly:
better worked technologies tend to have better cost profiles.  (Paper at 
http://rsta.royalsocietypublishing.org/content/370/1974/4263.full.pdf
)

My fear is that the analysis in your paper suffers this problem particularly as 
regards gun technology.  You consider (briefly) hydrogen guns - but these are 
not necessary for the altitudes you try to reach.  Methane-air or 
Methane-oxygen is adequate. These do not appear to have been discussed at all. 
Hydrogen guns do indeed have significant advantages for high altitude or 
widely-dispersed payloads, as their muzzle velocity is so high.  But methane 
propellant is comparable to the Mk7 charge in terms of performance, and is 
vastly cheaper. N.B.  I've spoken to industry experts too when developing my 
arguments - most notably Utron.

The other major cost in the gun system is the projectile.  Blackstock notes the 
opportunity for substantial costs savings (due to mass
production) in the Novim report, and there are additional possibilities for 
cost-cutting by recovery, such as parachute recovery, splashdown, etc., which 
can potentially reduce the costs of projectiles by an order of magnitude or 
more if reuse is practical.

Furthermore, guns generally offer substantial performance advantages in terms 
of their ability to deal with high-altitude dispersal and distribution through 
problematic weather conditions - something which may severely affect airships 
particularly.

In summary, therefore: the paper is great at bringing forward proposals for 
optimised aircraft (inc. airships).  However, it does not satisfactorily 
consider other technologies (e.g. guns), and therefore should not be used to 
make an economic case against these technologies.

Thanks

A


On 5 September 2012 13:56, David Keith david_ke...@harvard.edu wrote:
 Andrew



 Answers to your questions about the our recent URL paper on 
 stratospheric albedo modification delivery systems.



 Q: Isn't this just a reformatted version of the Aurora flight report?

 A: Essentially yes

RE: [geo] David Keith New Mexico experiment, press reaction

2012-07-17 Thread David Keith
Despite the quotes Martin Lukacs the reporter for the Guardian did not talk to 
either Jim Anderson or me in reporting this story.

The story is incorrect in several crucial ways. First and most important no 
experiment is definitely planed or funded.

It's true that we are in the early stages of planning and experiment to look at 
aerosol and ozone science questions, and that one of the topics we will address 
is risks of aerosol SRM. A balloon based platform is one of the possible 
methods. But, there is no possibility that it will go forward within a year as 
claimed in the article. Moreover, I would only support and participate in such 
an experiment if (a) it's funding was substantially public and (b) it was 
supported and approved by relevant public science research agencies, and (c) it 
provided a real opportunity to advance our understanding of the risk or 
efficacy of SRM.

While this story appears in a reputable paper has the appearance of primary 
reporting, it seems to have been assembled from fragments found on the web 
without even the most basic fact-checking.

David


From: geoengineering@googlegroups.com [mailto:geoengineering@googlegroups.com] 
On Behalf Of Andrew Lockley
Sent: Tuesday, July 17, 2012 12:01 PM
To: geoengineering@googlegroups.com
Subject: [geo] David Keith New Mexico experiment, press reaction


http://m.guardian.co.uk/environment/2012/jul/17/us-geoengineers-spray-sun-balloon?cat=environmenttype=article

US geoengineers to spray sun-reflecting chemicals from balloon

Experiment in New Mexico will try to establish the possibility of cooling the 
planet by dispersing sulphate aerosols

Martin Lukacs
guardian.co.ukhttp://guardian.co.uk, Tuesday 17 July 2012

The field experiment in solar geoengineering aims to ultimately create a 
technology to replicate the observed effects of volcanoes that spew sulphates 
into the stratosphere.

Two Harvard engineers are to spray sun-reflecting chemical particles into the 
atmosphere to artificially cool the planet, using a balloon flying 80,000 feet 
over Fort Sumner, New Mexico.

The field experiment in solar geoengineering aims to ultimately create a 
technology to replicate the observed effects of volcanoes that spew sulphates 
into the stratosphere, using sulphate aerosols to bounce sunlight back to space 
and decrease the temperature of the Earth.

David Keith, one of the investigators, has argued that solar geoengineering 
could be an inexpensive method to slow down global warming, but other 
scientists warn that it could have unpredictable, disastrous consequences for 
the Earth's weather systems and food supplies. Environmental groups fear that 
the push to make geoengineering a plan B for climate change will undermine 
efforts to reduce carbon emissions.

Keith, who manages a multimillion dollar geoengineering research fund provided 
by Microsoft founder Bill Gates, previously commissioned a study by a US 
aerospace company that made the case for the feasibility of large-scale 
deployment of solar geoengineering technologies.

His US experiment, conducted with American James Anderson, will take place 
within a year and involve the release of tens or hundreds of kilograms of 
particles to measure the impacts on ozone chemistry, and to test ways to make 
sulphate aerosols the appropriate size. Since it is impossible to simulate the 
complexity of the stratosphere in a laboratory, Keith says the experiment will 
provide an opportunity to improve models of how the ozone layer could be 
altered by much larger-scale sulphate spraying.

The objective is not to alter the climate, but simply to probe the processes 
at a micro scale, said Keith. The direct risk is very small.

While the experiment may not harm the climate, environmental groups say that 
the global environmental risks of solar geoengineering have been amply 
identified through modelling and the study of the impacts of sulphuric dust 
emitted by volcanoes.

Impacts include the potential for further damage to the ozone layer, and 
disruption of rainfall, particularly in tropical and subtropical regions - 
potentially threatening the food supplies of billions of people, said Pat 
Mooney, executive director of the Canadian-based technology watchdog ETC Group. 
It will do nothing to decrease levels of greenhouse gases in the atmosphere or 
halt ocean acidification. And solar geoengineering is likely to increase the 
risk of climate-related international conflict - given that the modelling to 
date shows it poses greater risks to the global south.

A scientific study published last month concluded that solar radiation 
management could decrease rainfall by 15% in areas of North America and 
northern Eurasia and by more than 20% in central South America.

Last autumn, a British field test of a balloon-and-hosepipe device that would 
have pumped water into the sky generated controversy. The government-funded 
project - Stratospheric Particle Injection for Climate Engineering (Spice

RE: [geo] David Keith New Mexico experiment, press reaction

2012-07-17 Thread David Keith
Folks

My error. Looking through my records I find that I did talk with Martin Lukacs 
when he called reporting a story for the Toronto Star.

The story is erroneous in the ways I described below, but I was in error in 
saying that I never talked to Lukacs.

David


From: David Keith
Sent: Tuesday, July 17, 2012 12:18 PM
To: 'andrew.lock...@gmail.com'; geoengineering@googlegroups.com
Subject: RE: [geo] David Keith New Mexico experiment, press reaction

Despite the quotes Martin Lukacs the reporter for the Guardian did not talk to 
either Jim Anderson or me in reporting this story.

The story is incorrect in several crucial ways. First and most important no 
experiment is definitely planed or funded.

It's true that we are in the early stages of planning and experiment to look at 
aerosol and ozone science questions, and that one of the topics we will address 
is risks of aerosol SRM. A balloon based platform is one of the possible 
methods. But, there is no possibility that it will go forward within a year as 
claimed in the article. Moreover, I would only support and participate in such 
an experiment if (a) it's funding was substantially public and (b) it was 
supported and approved by relevant public science research agencies, and (c) it 
provided a real opportunity to advance our understanding of the risk or 
efficacy of SRM.

While this story appears in a reputable paper has the appearance of primary 
reporting, it seems to have been assembled from fragments found on the web 
without even the most basic fact-checking.

David


From: geoengineering@googlegroups.commailto:geoengineering@googlegroups.com 
[mailto:geoengineering@googlegroups.com]mailto:[mailto:geoengineering@googlegroups.com]
 On Behalf Of Andrew Lockley
Sent: Tuesday, July 17, 2012 12:01 PM
To: geoengineering@googlegroups.commailto:geoengineering@googlegroups.com
Subject: [geo] David Keith New Mexico experiment, press reaction


http://m.guardian.co.uk/environment/2012/jul/17/us-geoengineers-spray-sun-balloon?cat=environmenttype=article

US geoengineers to spray sun-reflecting chemicals from balloon

Experiment in New Mexico will try to establish the possibility of cooling the 
planet by dispersing sulphate aerosols

Martin Lukacs
guardian.co.ukhttp://guardian.co.uk, Tuesday 17 July 2012

The field experiment in solar geoengineering aims to ultimately create a 
technology to replicate the observed effects of volcanoes that spew sulphates 
into the stratosphere.

Two Harvard engineers are to spray sun-reflecting chemical particles into the 
atmosphere to artificially cool the planet, using a balloon flying 80,000 feet 
over Fort Sumner, New Mexico.

The field experiment in solar geoengineering aims to ultimately create a 
technology to replicate the observed effects of volcanoes that spew sulphates 
into the stratosphere, using sulphate aerosols to bounce sunlight back to space 
and decrease the temperature of the Earth.

David Keith, one of the investigators, has argued that solar geoengineering 
could be an inexpensive method to slow down global warming, but other 
scientists warn that it could have unpredictable, disastrous consequences for 
the Earth's weather systems and food supplies. Environmental groups fear that 
the push to make geoengineering a plan B for climate change will undermine 
efforts to reduce carbon emissions.

Keith, who manages a multimillion dollar geoengineering research fund provided 
by Microsoft founder Bill Gates, previously commissioned a study by a US 
aerospace company that made the case for the feasibility of large-scale 
deployment of solar geoengineering technologies.

His US experiment, conducted with American James Anderson, will take place 
within a year and involve the release of tens or hundreds of kilograms of 
particles to measure the impacts on ozone chemistry, and to test ways to make 
sulphate aerosols the appropriate size. Since it is impossible to simulate the 
complexity of the stratosphere in a laboratory, Keith says the experiment will 
provide an opportunity to improve models of how the ozone layer could be 
altered by much larger-scale sulphate spraying.

The objective is not to alter the climate, but simply to probe the processes 
at a micro scale, said Keith. The direct risk is very small.

While the experiment may not harm the climate, environmental groups say that 
the global environmental risks of solar geoengineering have been amply 
identified through modelling and the study of the impacts of sulphuric dust 
emitted by volcanoes.

Impacts include the potential for further damage to the ozone layer, and 
disruption of rainfall, particularly in tropical and subtropical regions - 
potentially threatening the food supplies of billions of people, said Pat 
Mooney, executive director of the Canadian-based technology watchdog ETC Group. 
It will do nothing to decrease levels of greenhouse gases in the atmosphere or 
halt ocean acidification. And solar geoengineering is likely

[geo] New paper: Juan B Moreno-Cruz and David W Keith Climate Policy under Uncertainty: A Case for Geoengineering

2012-07-13 Thread David Keith
Juan B Moreno-Cruz and David W Keith. (2012). Climate Policy under Uncertainty: 
A Case for Geoengineering. Climatic Change, DOI 10.1007/s10584-012-0487-4.

Available at http://www.springerlink.com/content/l824m4unw0472803/fulltext.pdf
N.B., Almost all my papers are available at 
http://www.keith.seas.harvard.edu/geo.html. Some need a password, but all you 
have to do to get it is to send email to Hollie Roberts at 
rober...@ucalgary.camailto:rober...@ucalgary.ca. I also put a bunch of 
video's up on the site including this interview on HardTalk on of the BBC's 
leading interview programs: 
http://www.youtube.com/watch?v=dJTpZgubtPkfeature=youtu.be. See also: 
http://blogs.nature.com/from_the_lab_bench/2012/06/24/the-gatekeepers-of-sunlight


Juan B Moreno-Cruz and David W Keith,
Abstract:
Abstract Solar Radiation Management (SRM) has two characteristics that make it 
useful for managing climate risk: it is quick and it is cheap. SRM cannot, 
however, perfectly offset CO2-driven climate change, and its use introduces 
novel climate and environmental risks. We introduce SRM in a simple economic 
model of climate change that is designed to explore the interaction between 
uncertainty in the climate's response to CO2 and the risks of SRM in the face 
of carbon-cycle inertia. The fact that SRM can be implemented quickly, reducing 
the effects of inertia, makes it a valuable tool to manage climate risks even 
if it is relatively ineffective at compensating for CO2-driven climate change 
or if its costs are large compared to traditional abatement strategies. 
Uncertainty about SRM is high, and decision makers must decide whether or not 
to commit to research that might reduce this uncertainty. We find that even 
modest reductions in uncertainty about the side effects of SRM can reduce the 
overall costs of climate change in the order of 10%.


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RE: [geo] Mixing of sulphur precursor gases + Response to Simone

2012-07-13 Thread David Keith
Andrew



Dipping into this list after a long time ignoring it.



You asked: One thing which I personally am currently unclear on is the optimal 
microscale mixing ratios required.  Has anyone considered the effect of a dense 
injection regime, e.g. a balloon or slurry pipe, versus a distributed regime, 
e.g. an aircraft fleet?



Simone Tilmes said I think it is important to point out that there is very 
likely a limit on how much the Earth's surface could be cooled using sulfate 
aerosols, due to coagulation processes and fall out of aerosols. Only less than 
2 W/m2 reduction of global net surface SW flux was achieved in the study by 
Heckendorn et al., 2009, using a micro-physical model to consider size 
distributions of the aerosols. Niemeier et al., 2010, achieved a stronger 
forcing if injecting particles at 30hPa, which allow them to stay longer in the 
stratosphere. Though it will be hard to inject particles that high.



Small scale mixing is exactly what we focused on in: Jeffrey R. Pierce, Debra 
K. Weisenstein, Patricia Heckendorn, Thomas Peter and David W. Keith. (2010). 
Efficient formation of stratospheric aerosol for geoengineering by emission of 
condensible vapor from aircraft. Geophysical Research Letters, 37, L18805, 
doi:10.1029/2010GL043975. (PDF with no password needed)



The point of this paper is that releasing H2SO4 vapor in plumes that are 
rapidly mixed allows production of sulfate aerosol with effective size 
distribution. We coupled a small-scale plume to a global model and found that, 
in our model, much less sulfate was required to get radiative forcings of a few 
Wm^-2 that is required with the SO2 method. (E.g., to get 4 Wm^-2 one needs 
about 8 Mt-S/year with this 'direct aerosol method' versus 20 with SO2.)



This method would not work with balloon pipes (assuming reasonable limits on 
the number of pipes) because dispersal rates must be too big for the H2SO4 
vapor route to work.



Moreover, we also looked a various SO2 schemes and we do find that reasonably 
even distribution is important to avoid the big droplet problem.



English, Toon and Mill's found similar results with respect to the need for 
broad dispersal of SO2  
http://www.atmos-chem-phys.net/12/4775/2012/acp-12-4775-2012.pdf. At first 
glance this paper appears to contradict ours on utility of direct H2SO4 
injection, but on close inspection I think it shows strong agreement. They 
found that H2SO4 emitted in dispersed from-that is mixed at the grid-box 
level-has no advantage. This is exactly what one would expect since from the 
aerosols microphysics is just like the production of H2SO4 by oxidation of SO2. 
My understanding is that subsequent e-mail exchanges between English and Pierce 
have clarified that there is no essential disagreement on this point. Indeed 
it's not clear if there's any way that one could disperse H2SO4 evenly in a way 
that matched the simulation of English et al.



David



-Original Message-
From: geoengineering@googlegroups.commailto:geoengineering@googlegroups.com 
[mailto:geoengineering@googlegroups.com]mailto:[mailto:geoengineering@googlegroups.com]
 On Behalf Of Andrew Lockley
Sent: Tuesday, June 05, 2012 7:18 PM
To: geoengineering
Subject: [geo] Mixing of sulphur precursor gases



Hi



This paper is well worth reading



Heckendorn, P.; Weisenstein, D.; Fueglistaler, S.; Luo, B. P.; Rozanov, E.; 
Schraner, M.; Thomason, L. W.; Peter, T. (2009). The impact of geoengineering 
aerosols on stratospheric temperature and ozone. Environmental Research 
Letters 4: 045108.

Bibcode2009ERL.4d5108H. doi:10.1088/1748-9326/4/4/045108



The authors consider the temporal and spatial injection regime best suited to 
attaining well-mixed sulphur particles of the correct size distribution for 
geoengineering use.  They conclude that spatial distribution is helpful, but 
temporal distribution is unhelpful.  I personally would welcome list discussion 
on whether this conclusion is seen as reliable, and additionally clarification 
of the processes involved.



One thing which I personally am currently unclear on is the optimal microscale 
mixing ratios required.  Has anyone considered the effect of a dense injection 
regime, e.g. a balloon or slurry pipe, versus a distributed regime, e.g. an 
aircraft fleet?  Heckendorn do not seem to have addressed this issue at all in 
their paper.



It's unclear to me whether the injection density on a scale of 10E1-10E4m would 
be significant in the formation of aerosols.  I'm not aware of any paper which 
considers this microscale mixing.



Any links  comments are appreciated.



A



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RE: [geo] Regional SRM experiment

2012-05-01 Thread David Keith
Folks

I am not getting this, and yet I am close to it. My office is down the hall 
from the GEOS-Chem group that produced these papers. We collaborate in that 
Debra Weisenstein works with me and with that group is doing  modeling for 
geoengineering and looking into improvements to the GEOS-Chem stratospheric 
chemistry.

1. Can someone tell me exactly what would be tested here? Climate response? 
Aerosol radiative forcing?

2. Is there a sensible reason why you one would prefer troposphere SO2 for 
geoengineering if one wanted to do it? Recall that trop SO2 now is linked to 
about 1 million air pollution deaths per year globally as well as acid rain etc.

3. The idea that cutting tropospheric SO2 pollution is a form of geoengineering 
would seem to me to extend the definition of geoengineering to mean, in effect, 
any human action that may alter the climate. I doubt this definition will 
help clarify debate.

Yours,
David




From: geoengineering@googlegroups.com [mailto:geoengineering@googlegroups.com] 
On Behalf Of Hawkins, Dave
Sent: Tuesday, May 01, 2012 10:51 AM
To: natcurr...@gmail.com; geoengineering@googlegroups.com
Cc: mmacc...@comcast.net
Subject: RE: [geo] Regional SRM experiment


Nathan,

The CEC report you link to was useful but is now dated.  Much more current 
information on SO2 emissions (up to and including 4th quarter 2011 for the 
power sector) is available thanks to the 1990 Clean Air Act, which required SO2 
continuous emission monitors on all coal power plants in the 48 contiguous 
states of the US.

A handy spreadsheet of national SO2 emission trends from 1980 to 2010 can be 
found here:

http://www.epa.gov/airmarkets/progress/ARPCAIR_downloads/CAIR_ARP_2010_data_1.xls

This spreadsheet also includes data disaggregated by state and by month.

Other pages at the airmarkets link above will get you access to hourly 
emissions and operational data from all significant US coal power plants.  
(FWIW, getting the rules in place to require these data to be reported at all, 
much less to be reported electronically and accessible to anyone, required 
quite a lot of persistent advocacy.)

The national SO2 trends are informative as to the scale of the reductions from 
more than 17 million tons of SO2 from the power sector in 1980 to about 5.2 
million tons in 2010.  The combination of EPA's new transport rule and toxics 
rule will cut the load further to about 2 million tons in the 2015-2016 time 
frame.  http://www.epa.gov/ttn/ecas/regdata/RIAs/matsriafinal.pdf, Table 3-4.

But the additional instrumentation I was referring to in  my email was not 
emission monitoring data (as the above information indicates, we now have that 
pretty well in place in the US for the power sector).  Rather, I am thinking of 
high resolution data of the characteristics of the atmosphere that might change 
as these additional emission reduction occur.  I don't know enough to have 
anything in particular in mind but I imagine there are some on this list who 
could identify the data sets they would like to have to fully characterize the 
forcing and other aspects of the changes brought about by the large SO2 
reductions from 1980 to date and from the large additional percentage 
reductions that will occur over the next 3-5 years.  For example, how linear or 
nonlinear are the forcing responses to a given tonnage reduction in fine 
particle precursors or a given ppm change in fine particle concentrations.  My 
hunch is that the localized impacts will differ depending on the baseline 
atmospheric conditions on which the emission changes are imposed.  Knowing more 
about that might be nice to help improve modeling estimates of the 
local/regional impacts of SRM experiments.

David

From: geoengineering@googlegroups.commailto:geoengineering@googlegroups.com 
[mailto:geoengineering@googlegroups.com] On Behalf Of Nathan Currier
Sent: Tuesday, May 01, 2012 11:38 AM
To: geoengineering@googlegroups.commailto:geoengineering@googlegroups.com
Cc: mmacc...@comcast.netmailto:mmacc...@comcast.net; Geoengineering
Subject: Re: [geo] Regional SRM experiment

Hi, David -

I fully agree with that, and actually used that same MIT paper in something
I wrote up for the group AMEG recently. In fact, if you look at table 3.3 in 
this -

http://www.findthatfile.com/search-19564999-hPDF/download-documents-4876_powerplant_airemission_en.pdf.htm

you'll also see that of the top 10 highest SO2-producing
power plants in the US - and these are the only US plants that put out
over 100,000 mt SO2/yr each (and their inputs get smaller pretty quickly as
the sizes decrease) -  7 of the 10 are just in Penn  OH alone.
On the dot map of US SO2 emissions in the attached, these two states are
almost invisible, being swallowed up by a big dot for all the SO2 there.
I don't have a figure for the average loading of the two states, but it
could be roughly ascertained pretty easily by EPA's SO2 trends map.

Anyhow, just a study of the SO2 in these two 

RE: [geo] Good popsci article on key SRM facilitator tech

2012-05-01 Thread David Keith
Agreed with John here.

Why was this posted at all? Given (a) that conventional aircraft engines can 
get sulfate and other aerosols to altitudes above 20 km, and that (b) both 
models and basic understanding of stratospheric circulation suggests this is a 
sufficient altitude.

This list would be more useful if the posts had a higher signal-to-noise ratio.

David


-Original Message-
From: geoengineering@googlegroups.com [mailto:geoengineering@googlegroups.com] 
On Behalf Of John Latham
Sent: Friday, April 27, 2012 9:09 AM
To: s.sal...@ed.ac.uk; geoengineering@googlegroups.com
Subject: RE: [geo] Good popsci article on key SRM facilitator tech

Hello Andrew,

Not sure if this is the same point as that made by Steve below.

Please dont call stratospheric sulphur seeding SRM. The implicit message 
conveyed by doing so is that there is only one SRM scheme whereas in fact there 
are several. Sulphur seeding is the best recognised and best supported SRM 
idea. It can easily handle having a few neighbours.

You are of course not the only one who doesnt make this distiction.

All Best Wishes,   John.



John Latham
Address: P.O. Box 3000,MMM,NCAR,Boulder,CO 80307-3000
Email: lat...@ucar.edu  or john.latha...@manchester.ac.uk
Tel: (US-Work) 303-497-8182 or (US-Home) 303-444-2429
 or   (US-Cell)   303-882-0724  or (UK) 01928-730-002
http://www.mmm.ucar.edu/people/latham

From: geoengineering@googlegroups.com [geoengineering@googlegroups.com] on 
behalf of Stephen Salter [s.sal...@ed.ac.uk]
Sent: Friday, April 27, 2012 3:40 PM
To: geoengineering@googlegroups.com
Subject: Re: [geo] Good popsci article on key SRM facilitator tech

  Andrew

May I suggest the insertion of the word 'stratospheric' before SRM in your last 
email.

Stephen

Emeritus Professor of Engineering Design Institute for Energy Systems School of 
Engineering Mayfield Road University of Edinburgh EH9  3JL Scotland Tel +44 131 
650 5704 Mobile 07795 203 195 www.see.ed.ac.uk/~shs


On 27/04/2012 15:27, Andrew Lockley wrote:

 Mech eng fans will be interested in this great article on high 
 altitude engines, which have potential for application to the heavy, 
 high altitude lift needed for SRM.

 Please view online to access rich media.

 http://www.bbc.co.uk/news/science-environment-17864782

 A

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 UK engineers have begun critical tests on a new engine technology 
 designed to lift a spaceplane into orbit.

 The proposed Skylon vehicle would operate like an airliner, taking off 
 and landing at a conventional runway.

 Its major innovation is the Sabre engine, which can breathe air like a 
 jet at lower speeds but switch to a rocket mode in the high atmosphere.

 Reaction Engines Limited (REL) believes the test campaign will prove 
 the readiness of Sabre's key elements.

 This being so, the firm would then approach investors to raise the 
 £250m needed to take the project into the final design phase.

 We intend to go to the Farnborough International Air Show in July 
 with a clear message, explained REL managing director Alan Bond.

 The message is that Britain has the next step beyond the jet engine; 
 that we can reduce the world to four hours - the maximum time it would 
 take to go anywhere. And that it also gives us aircraft that can go 
 into space, replacing all the expendable rockets we use today.

 To have a chance of delivering this message, REL's engineers will need 
 a flawless performance in the experiments now being run on a rig at 
 their headquarters in Culham, Oxfordshire.

 The test stand will not validate the full Sabre propulsion system, but 
 simply its enabling technology - a special type of pre-cooler heat 
 exchanger.

 Sabre is part jet engine, part rocket engine. It burns hydrogen and 
 oxygen to provide thrust - but in the lower atmosphere this oxygen is 
 taken from the atmosphere.

 The approach should save weight and allow Skylon to go straight to 
 orbit without the need for the multiple propellant stages seen in 
 today's throw-away rockets.

 But it is a challenging prospect. At high speeds, the Sabre engines 
 must cope with 1,000-degree gases entering their intakes. These need 
 to be cooled prior to being compressed and burnt with the hydrogen.

 Reaction Engines' breakthrough is a module containing arrays of 
 extremely fine piping that can extract the heat and plunge the intake 
 gases to minus 140C in just 1/100th of a second.

 Ordinarily, the moisture in the air would be expected to freeze out 
 rapidly, covering the pre-cooler's pipes in a blanket of frost and 
 compromising their operation.

 But the REL team has also devised a means to stop this happening, 
 permitting Sabre to run in jet mode for as long as is needed before 
 making the transition to a booster rocket.

 Sabre 

[geo] RE: Rough sketch of a small-scale tropospheric aerosol program

2012-03-21 Thread David Keith
Folks

Part of this thread is spinning into an exercise in drafting a statement. I 
suggest that this activity move off-line to a smaller group.

A few specific comments:

1. “we have a method that does not use sulphur”. Maybe. As a method of SRM, sea 
salt aerosols offer many potential advantages and some serious disadvantages.  
For this reason I strongly support research including active field research. 
But, there are still **very** large uncertainties and it is entirely possible 
that the method will prove to have very limited applicability.

Over hype of high-leverage technologies is a recipe for disaster.

2. Stratospheric sulfates are plausible because (a) we know how to deliver 
sulfate at low cost with current technologies and (b) the experience with 
volcanic emissions gives us some confidence that we understand some of the key 
chemistry and physics. There will still be unexpected outcomes.

Here is a specific example. I you wanted to increase the radiative forcing 
using strat sulfate aerosols at a rate sufficient to roughly offset the growth 
of anthropogenic radiative forcing you would need ramp up the sulfate addition 
rate at about 1/3 of a Mt-S per decade. That is if you started at zero you 
would need about 1/3 of a Mt-S per year after a decade and 2/3 after two 
decades. (This assumes 0.25 Wm^-2/decade forcing ramp and 0.7 Wm^-2 for 1 
Mt-S/year see; Pierce et al, 
http://www.keith.seas.harvard.edu/preprints/127.Pierce.EfficientFormStratsAerosol.p.pdf)

Sulfate aerosols in the stratosphere are promising. I would not support 
deployment without a much broader effort on both science and governance, but 
with luck, I think this could be accomplished reasonably quickly.

There are lots of other options that offer similar promise. We are spending 
considerable effort thinking about how to increase the effectiveness and 
understand the risks of sulfate and other aerosols.

3. Tropospheric sulfates require much large injection rates to achieve the same 
radiative forcing. Do the math on health impacts using paper I cited a few 
posts back. It’s not promising. I would respectfully suggest that one be 
cautious about propose something that will have health consequences that large 
without a **very** clear rational for why you are doing it.

David






From: Tenney Naumer [mailto:alais.el...@gmail.com]
Sent: Wednesday, March 21, 2012 8:06 PM
To: Mike MacCracken
Cc: P. Wadhams; Nathan Currier; Geoengineering; Andrew Lockley; 
john.latha...@manchester.ac.uk; Govindasamy Bala; Veli Albert Kallio; David 
Keith; v.ga...@open.ac.uk; John Nissen; Peter R Carter; Gary Houser; Anthony 
Cook; Graham Innes; PaulHenry Beckwith; Brian Orr; JON HUGHES; Nick Breeze
Subject: Re: Rough sketch of a small-scale tropospheric aerosol program

Dear Mike,

I think the point is that we have a method that does not use sulphur.

The fact that many people are exposed to atmospheric sulphur now is no logical 
justification for its use in geoengineering.

We need cleaner air in general.

World governments need to invest in methods for drawing down CO2 and rid the 
air of other man-caused aerosols.

Why exacerbate a problem that we will have to work extra hard to clean up later?

Best regards,

Tenney

Tenney Naumer  Climate Change: The Next 
Generationhttp://climatechangepsychology.blogspot.com
Tel.: (618) 967-6453 (cell)
skype:  tenneynaumer


On Wed, Mar 21, 2012 at 3:45 PM, Mike MacCracken 
mmacc...@comcast.netmailto:mmacc...@comcast.net wrote:
Peter and Tenney--

I think your proposed proscription of sulfur is too harsh a restriction. As
far as people are concerned, the problems have come with high concentrations
and lots of other toxins mixed with them from fossil fuel power plants. As
far as ecological impacts are concerned, aside from there being agricultural
areas that are sulfur deficient and farmers add sulfur, the problems arise
in certain types of situations (like accumulated deposition onto the snow
fields of Scandinavia and then rapid melting; downwind of major
industrialized areas; etc). In any case, as well, we will continue to have
volcanic injections so sulfur won't be going away.

On low sulfur fuel, that is mandated to happen over next several years,
mainly because of problematic emissions and concentrations in port areas.
This is likely, however, to have much larger scale implications as the
diesel fuel is cleaned up.

CCN approach and cloud whitening is great to try, but is mainly effective in
clean areas where there is marine stratus and and a bit hard to do in other
areas where that is not the case.

Thinking that one is going to find an approach that has no side effects of
any kind is, in my view, wishing for the impossible. It is, as I posed in an
earlier email, like insisting on a cure for HIV/AIDS rather than accepting
drugs that are able to hold off worsening of the disease while one searches
for better approaches.

Mike MacCracken



On 3/21/12 1:59 PM, P. Wadhams p...@cam.ac.ukmailto:p

RE: [geo] Source on SRM causing warming

2012-03-19 Thread David Keith
And... this 2-4 month lifetime is very altitude and latitude dependent.

We can run some sims with the AER 2D an look but my guess from what we have 
done is that you could make choices that would push this up a bit.

David


From: geoengineering@googlegroups.com [mailto:geoengineering@googlegroups.com] 
On Behalf Of Alan Robock
Sent: Monday, March 19, 2012 10:03 AM
To: mmacc...@comcast.net
Cc: Stephen Salter; Ken Caldeira; Andrew Lockley; Geoengineering; 
j.e.kristjans...@geo.uio.no
Subject: Re: [geo] Source on SRM causing warming

Dear Mike,

I don't know how you do this 6 to 1 calculation.  We found that the e-folding 
time for stratospheric aerosols in the Arctic s 2-4 months, with 4 months in 
the summer, the relevant time.  (see 
http://climate.envsci.rutgers.edu/pdf/2008JD010050small.pdf )  If we compare 
this to the lifetime of tropospheric aerosols, on week, and add a week to the 4 
months for their tropospheric time, the ratio is 130 days to 7 days, which is 
19 to 1, not 6 to 1.  Furthermore, the health effects of additional 
tropospheric pollution are not acceptable, in my opinion.




Alan



[On sabbatical for current academic year.  The best way to contact me

is by email, rob...@envsci.rutgers.edumailto:rob...@envsci.rutgers.edu, or at 
732-881-1610 (cell).]



Alan Robock, Professor II (Distinguished Professor)

  Editor, Reviews of Geophysics

  Director, Meteorology Undergraduate Program

  Associate Director, Center for Environmental Prediction

Department of Environmental SciencesPhone: +1-732-932-9800 x6222

Rutgers University  Fax: +1-732-932-8644

14 College Farm Road   E-mail: 
rob...@envsci.rutgers.edumailto:rob...@envsci.rutgers.edu

New Brunswick, NJ 08901-8551  USA  http://envsci.rutgers.edu/~robock

On 3/18/2012 5:49 PM, Mike MacCracken wrote:

Hi Stephen--My wording must have been confusing.



For stratospheric injections at low latitudes, the lifetime is 1-2 years.

The aerosols do move poleward and are carried into the troposphere in mid

and high latitudes. This is one approach to trying to limit global climate

change, and, as David Keith says, studies indicate that these cool the polar

regions, though perhaps not in the stratosphere.



Your cloud brightening approach is also to limit global warming. I'd also

suggest that we could offset some of the global warming by sulfate aerosols

out over vast ocean areas instead of sulfate's present dominance over, now,

southeastern Asia, China, etc.--so keeping or modestly enhancing the present

cooling offset. [And reducing cirrus may also be a viable approach.]



A third approach is to cool the poles (and this might be good for regional

purposes alone), but cooling also pulls heat out of lower latitudes and

helps to cool them somewhat. The Caldeira-Wood shows it works conceptually

(they reduced solar constant) and Robock et al. injected SO2 into

stratosphere to do (but the full year injection of SO2/SO4 likely spread

some to lower latitudes and the monsoons were affected). One thing Robock et

al. found was that the lifetime of sulfate in the polar stratosphere is

about two months, and so that means that the potential 100 to 1 advantage of

stratospheric sulfate is not valid, and we're down to 6 to 1 compared to

surface-based approaches such as CCN or microbubbles to cool incoming

waters, sulfate or something similar over Arctic area, surface brightening

by microbubbles, etc.--noting that such approaches are only needed (and

effective) for the  few months per year when the Sun is well up in the sky.



As David Keith also says, there is a lot of research to be done to determine

which approaches or alone or in different variants might work, or be

effective or ineffective and have unintended consequences, much less how

such an approach or set of approaches might be integrated with mitigation,

adaptation, suffering, etc.



Best, Mike MacCracken













On 3/18/12 12:52 PM, Stephen Salter 
s.sal...@ed.ac.ukmailto:s.sal...@ed.ac.uk wrote:



Mike



I had thought that the plan was stratospheric aerosol to be released at

low latitudes and would slowly migrate to the poles where is would

gracefully descend.  If you can be sure that it will all have gone in 10

days then my concerns vanish.  But if the air cannot get through the

water surface how can the aerosol it carries get there?  It will form a

blanket even if it is a very low one.



A short life would mean  that we do not have to worry about methane

release.  But can we do enough to cool the rest of the planet?  Perhaps

Jon Egil can tell us about blanket lifetime.



Stephen



Mike MacCracken wrote:

The Robock et al simulations of an Arctic injection found that the lifetime

of particles in the lower Arctic stratosphere was only two months. In that

one would only need particles up during the sunlit season (say three months,

for only really helps after the sea ice surface has melted

RE: [geo] Source on SRM causing warming

2012-03-19 Thread David Keith
 Keith says, studies indicate that these cool the polar
regions, though perhaps not in the stratosphere.

Your cloud brightening approach is also to limit global warming. I'd also
suggest that we could offset some of the global warming by sulfate aerosols
out over vast ocean areas instead of sulfate's present dominance over, now,
southeastern Asia, China, etc.--so keeping or modestly enhancing the present
cooling offset. [And reducing cirrus may also be a viable approach.]

A third approach is to cool the poles (and this might be good for regional
purposes alone), but cooling also pulls heat out of lower latitudes and
helps to cool them somewhat. The Caldeira-Wood shows it works conceptually
(they reduced solar constant) and Robock et al. injected SO2 into
stratosphere to do (but the full year injection of SO2/SO4 likely spread
some to lower latitudes and the monsoons were affected). One thing Robock et
al. found was that the lifetime of sulfate in the polar stratosphere is
about two months, and so that means that the potential 100 to 1 advantage of
stratospheric sulfate is not valid, and we're down to 6 to 1 compared to
surface-based approaches such as CCN or microbubbles to cool incoming
waters, sulfate or something similar over Arctic area, surface brightening
by microbubbles, etc.--noting that such approaches are only needed (and
effective) for the  few months per year when the Sun is well up in the sky.

As David Keith also says, there is a lot of research to be done to determine
which approaches or alone or in different variants might work, or be
effective or ineffective and have unintended consequences, much less how
such an approach or set of approaches might be integrated with mitigation,
adaptation, suffering, etc.

Best, Mike MacCracken






On 3/18/12 12:52 PM, Stephen Salter s.sal...@ed.ac.uk 
mailto:s.sal...@ed.ac.uk  wrote:



Mike

I had thought that the plan was stratospheric aerosol to be released at
low latitudes and would slowly migrate to the poles where is would
gracefully descend.  If you can be sure that it will all have gone in 10
days then my concerns vanish.  But if the air cannot get through the
water surface how can the aerosol it carries get there?  It will form a
blanket even if it is a very low one.

A short life would mean  that we do not have to worry about methane
release.  But can we do enough to cool the rest of the planet?  Perhaps
Jon Egil can tell us about blanket lifetime.

Stephen

Mike MacCracken wrote:


The Robock et al simulations of an Arctic injection found that the lifetime
of particles in the lower Arctic stratosphere was only two months. In that
one would only need particles up during the sunlit season (say three months,
for only really helps after the sea ice surface has melted and the sun is
high in the sky). During the relatively calm weather of Arctic summer, the
lifetime of tropospheric sulfate, for exampleand quite possibly sea salt
CCN--emitted above the inversion is likely 10 days or so. It is not at all
clear to me that the 6 to 1 or so lifetime advantage of the lower
stratosphere is really worth the effort to loft the aerosols.

And on the temperature rise in the polar stratosphere, I would hope any
calculation of the effects of the sulfate/dust injection only put it in
during the sunlit seasonobviously, there would be no effect on solar
radiation during the polar night, so, with a two month lifetime of aerosols
there, it makes absolutely no sense to be lofting anything for about two
thirds of the year. And so likely no effect on winter temperatures (although
warming the coldest part of the polar winter stratosphere might well help to
prevent an ozone hole from forming).

So, I think a tropospheric brightening approach is likely the better option.
Whether it can be done with just CCN or might also need sulfate seems to me
worth investigating (what one needs may well be not just cloud brightening,
but also clear sky aerosol loading).

Best, Mike

*

On 3/17/12 8:41 PM, Ken Caldeira kcalde...@carnegie.stanford.edu 
mailto:kcalde...@carnegie.stanford.edu  wrote:




That is just misleading.  The third attachment is a top-of-atmosphere
radiation balance on the email I am responding to shows shortwave radiation.

The attached figure shows the corresponding temperature field from the same
simulation for the same time period.  Note Arctic cooling.

Also, we should not focus on individual regional blobs of color in an
average
of a single decade from a single simulation.

The paper these figures came from is here:
http://www.atmos-chem-phys.net/10/5999/2010/acp-10-5999-2010.pdf

___
Ken Caldeira

Carnegie Institution Dept of Global Ecology
260 Panama Street, Stanford, CA 94305 USA
+1 650 704 7212 kcalde...@carnegie.stanford.edu
http://dge.stanford.edu/labs/caldeiralab  @kencaldeira

YouTube:
 http://www.youtube.com/watch?v=a9LaYCbYCxo Climate change and the
transition from coal to low-carbon electricity
http://www.youtube.com/watch?v

RE: [geo] Re: We are top story on BBC environmental news

2012-03-18 Thread David Keith
John

Do you have a physically based model that backs up these about collapse and 
quadrupling of warming rate?

If so, please let us see it.

If not, please consider either retracting these claims or finding a way to make 
clear the level of uncertainty involved.

We have a climate problem and a public relations problem.

The first email I have from you in my archives is dated 2008 and suggests the 
complete disappearance of summer Arctic sea ice at the by 2013. This now seems 
highly unlikely.

If the current claims about immanent collapse are also proved false (as I 
expect they will be) you will provide ammunition to those who argue against 
action.

Reality is bad enough.

David

-Original Message-
From: geoengineering@googlegroups.com [mailto:geoengineering@googlegroups.com] 
On Behalf Of John Nissen
Sent: Sunday, March 18, 2012 11:24 AM
To: John Latham
Cc: johnnissen2...@gmail.com; joshuahorton...@gmail.com; geoengineering; P. 
Wadhams; Stephen Salter; JON HUGHES; Albert Kallio
Subject: Re: [geo] Re: We are top story on BBC environmental news


Dear John,

How I wish we had the time.  We should have been doing what you suggest 
immediately after the crash in sea ice extent of September 2007 - a
wake-up call.   We have just left it far too late, and have no option
but to try anything that might reduce the chance of a collapse in sea ice 
extent this year.  If you just look at the PIOMAS graph of sea ice volume which 
is down 75% in three decades and compare it with the sea ice extent which is 
down 40%, it is obvious that the sea ice extent cannot hold out much longer 
while the ice continues thinning.  There must be a great deal of heat going 
into melting the ice - and much of this heat is from the heating of open water 
by the sun when the sea ice
retreats - i.e. from the albedo flip effect.   After a collapse such
that there's little sea ice left in September, there will be a spurt in Arctic 
warming, perhaps to double the current rate of warming.  And after we have a 
nearly sea ice free Arctic ocean for six months, the warming could increase to 
triple or quadruple the current rate.
Meanwhile there is the methane to contend with.  There are already signs of an 
escalation of methane emissions from shallow seas of the continental shelf.  
That by itself would be cause for concern, since the sea ice retreat is 
allowing the seabed to warm well above the thaw point for methane hydrates.

So I have three questions for you:

1.  Do you seriously recommend that nobody does anything for at least three 
years while there is more research into geoengineering?

2.  How can you say that geoengineering is doomed to failure?  Do you really 
lack confidence in your own modelling?

3.  What do I tell my wife and children if nothing is done and the worst 
happens?

Kind regards,

John

---

On 18/03/2012 15:29, John Latham wrote:
 Hello John Nissen and All,

 John N says:-

 Just before the hearing, the committee had received an email
 [6] from some geoengineering experts recommending research but
 suggesting that development and deployment of geoengineering
 techniques was premature, thus undermining the AMEG position.

 I was one of the signatories that John alluded to. I believe that each
 one of us feel it shameful and dangerous that that  research into
 promising SRM ideas has not been significantly financially supported.
 The major stages of the required research involve modelling,
 resolution of all technological questions, examination of - and
 international agreement on - possible adverse consequences of
 deployment, and the execution of (in the case of MCB, for example), of
 a limited area field-testing experiment. If the required funding was 
 available now I think I think all the above goals could be achieved in 5 
 years, perhaps even 3.

 At the moment these goals are far from being achieved. An attempt to
 successfully deploy now any likely SRM  technique would be doomed to
 failure. The technological questions have not been fully resolved - so
 it would not work - and there would be
 - in my opinion - an international outcry against deployment.

 We would be shooting ourselves in the foot, I think, if we tried to
 deploy now. If there was a major failure - which is likely - the
 response could be such as to prohibit further SRM work for a long
 time.We need to engage in crash programmes of research now, which
 means that we need immediately to obtain the required funding. [How, I dont 
 know, I'm afraid].

 All Best,  John (Latham)

 John Latham
 Address: P.O. Box 3000,MMM,NCAR,Boulder,CO 80307-3000
 Email: lat...@ucar.edu  or john.latha...@manchester.ac.uk
 Tel: (US-Work) 303-497-8182 or (US-Home) 303-444-2429
   or   (US-Cell)   303-882-0724  or (UK) 01928-730-002
 http://www.mmm.ucar.edu/people/latham
 
 From: geoengineering@googlegroups.com
 [geoengineering@googlegroups.com] on behalf of John Nissen
 [johnnissen2...@gmail.com]
 

RE: [geo] Source on SRM causing warming

2012-03-18 Thread David Keith
Steven

I am in favor of serious research on both strat aerosols and sea salt CCN.

Your comments suggest that you already know the outcome of that research. You 
may of course be correct, and in many ways I hope you are. I, however, see less 
basis for certainty. 

A few facts that seem relevant: 

1. All simulations of stratospheric aerosols of which I am aware do show an 
arctic cooling tendency and increase in sea ice extent. 

2. There is little reason to doubt that 1 Wm^2 radiative global forcing could 
be produce by sulfate aerosols using well understood technologies. (That is not 
a claim about risks and side effects, just about basic capability.) 

3. There are large uncertainties about the efficacy of sea salt CCN in 
producing radiative forcing. It will certainly work sometimes under some 
conditions, but we don't yet have a good quantitative understanding of extent 
of conditions in which it might work and therefore of the aggregate 
effectiveness. 

4. There are advantages and disadvantages to the fact that the sea salt CCN is 
more patchy.

Given this is seems to me hard to conclude that we know the answer yet.

Yours,
David






-Original Message-
From: geoengineering@googlegroups.com [mailto:geoengineering@googlegroups.com] 
On Behalf Of Stephen Salter
Sent: Sunday, March 18, 2012 10:52 AM
To: mmacc...@comcast.net
Cc: Ken Caldeira; Andrew Lockley; Geoengineering; j.e.kristjans...@geo.uio.no
Subject: Re: [geo] Source on SRM causing warming

Mike

I had thought that the plan was stratospheric aerosol to be released at low 
latitudes and would slowly migrate to the poles where is would gracefully 
descend.  If you can be sure that it will all have gone in 10 days then my 
concerns vanish.  But if the air cannot get through the water surface how can 
the aerosol it carries get there?  It will form a blanket even if it is a very 
low one.

A short life would mean  that we do not have to worry about methane release.  
But can we do enough to cool the rest of the planet?  Perhaps Jon Egil can tell 
us about blanket lifetime.

Stephen

Mike MacCracken wrote:
 The Robock et al simulations of an Arctic injection found that the 
 lifetime of particles in the lower Arctic stratosphere was only two 
 months. In that one would only need particles up during the sunlit 
 season (say three months, for only really helps after the sea ice 
 surface has melted and the sun is high in the sky). During the 
 relatively calm weather of Arctic summer, the lifetime of tropospheric 
 sulfate, for example‹and quite possibly sea salt CCN--emitted above 
 the inversion is likely 10 days or so. It is not at all clear to me 
 that the 6 to 1 or so lifetime advantage of the lower stratosphere is really 
 worth the effort to loft the aerosols.

 And on the temperature rise in the polar stratosphere, I would hope 
 any calculation of the effects of the sulfate/dust injection only put 
 it in during the sunlit season‹obviously, there would be no effect on 
 solar radiation during the polar night, so, with a two month lifetime 
 of aerosols there, it makes absolutely no sense to be lofting anything 
 for about two thirds of the year. And so likely no effect on winter 
 temperatures (although warming the coldest part of the polar winter 
 stratosphere might well help to prevent an ozone hole from forming).

 So, I think a tropospheric brightening approach is likely the better option.
 Whether it can be done with just CCN or might also need sulfate seems 
 to me worth investigating (what one needs may well be not just cloud 
 brightening, but also clear sky aerosol loading).

 Best, Mike

 *

 On 3/17/12 8:41 PM, Ken Caldeira kcalde...@carnegie.stanford.edu wrote:

   
 That is just misleading.  The third attachment is a top-of-atmosphere 
 radiation balance on the email I am responding to shows shortwave radiation.

 The attached figure shows the corresponding temperature field from 
 the same simulation for the same time period.  Note Arctic cooling.

 Also, we should not focus on individual regional blobs of color in an 
 average of a single decade from a single simulation.

 The paper these figures came from is here: 
 http://www.atmos-chem-phys.net/10/5999/2010/acp-10-5999-2010.pdf

 ___
 Ken Caldeira

 Carnegie Institution Dept of Global Ecology
 260 Panama Street, Stanford, CA 94305 USA
 +1 650 704 7212 kcalde...@carnegie.stanford.edu
 http://dge.stanford.edu/labs/caldeiralab  @kencaldeira

 YouTube:
  http://www.youtube.com/watch?v=a9LaYCbYCxo Climate change and the 
 transition from coal to low-carbon electricity 
 http://www.youtube.com/watch?v=a9LaYCbYCxo
 Crop yields in a geoengineered climate 
 http://www.youtube.com/watch?v=-0LCXNoIu-c




 On Sat, Mar 17, 2012 at 1:31 PM, Andrew Lockley 
 and...@andrewlockley.com
 wrote:
 
 Hi

 Here are some model outputs which Stephen sent me. These appear to 
 show localized arctic warming in geoengineering simulations. This 
 could be due to 

RE: [geo] tropospheric aerosol use

2012-03-15 Thread David Keith
Some simple math:

Global sulfur emissions into troposphere are about 50 Mt-S per year and they 
have a direct radiative forcing of about -0.4 Wm^-2.

These same sulfate aerosols kill about 1 million people per year.

Of course current emissions are concentrated where people are you the ratio of 
mortality to radiative forcing is larger than it would be if you were focused 
on radiative forcing with tropospheric sulfate. But it would still be big. 
Intercontinental transport of sulfate kills, see: 
http://meetings.copernicus.org/www.cosis.net/abstracts/EGU2007/05111/EGU2007-J-05111.pdf

If you want to make 1Wm^-2 of forcing with sulfate aerosol in the troposphere 
you might need of order 50 Mt-S per year, whereas in the stratosphere you might 
be able to get away with just over 1 Mt-S per year. (see #127 at 
http://www.keith.seas.harvard.edu/geo.html).

One might do some optimization, but the case here has been clear for a long 
time. We said some of this twenty years ago. See in the table in the following 
though many numbers now look out of date or wrong:
David W. Keith and Hadi Dowlatabadi (1992). A Serious Look at Geoengineering. 
Eos, Transactions American Geophysical Union, 73: 289-293. 
(PDF)http://www.keith.seas.harvard.edu/papers/09_Keith_1992_SeriousLookAtGeoeng_s.pdf

David



From: geoengineering@googlegroups.com [mailto:geoengineering@googlegroups.com] 
On Behalf Of Govindasamy Bala
Sent: Thursday, March 15, 2012 9:53 PM
To: natcurr...@gmail.com
Cc: geoengineering
Subject: Re: [geo] tropospheric aerosol use

Climate changes by Budyko, on page 244, discusses why tropospheric aerosols 
are not as effective as stratospheric aerosols for climate modification.
1) life time is only a couple of weeks
2) Particle size becomes too big quickly and hence not effective for scattering
3) Presence of clouds make them less effective
4) absorption by aerosols of near IR shortwave could partially cancel the 
cooling by scattering.

Bala
On Thu, Mar 15, 2012 at 9:53 PM, Nathan Currier 
natcurr...@gmail.commailto:natcurr...@gmail.com wrote:
Does anyone know of any published papers exploring the use of
tropospheric aerosol use?

cheers,

Nathan

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Best wishes,

---
Dr. G. Bala
Associate Professor
Center for Atmospheric and Oceanic Sciences
Indian Institute of Science
Bangalore - 560 012
India

Tel: +91 80 2293 3428
+91 80 2293 2075
Fax: +91 80 2360 0865
+91 80 2293 3425
Email: gb...@caos.iisc.ernet.inmailto:gb...@caos.iisc.ernet.in
 bala.govhttp://bala.gov@gmail.comhttp://gmail.com
Web:http://caos.iisc.ernet.in/faculty/gbala/gbala.html
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RE: [geo] Fwd: Better brush up on your lies

2012-02-11 Thread David Keith
Strongly agree.

My experience talking with chemtrails folks a good fraction are positive and 
well intentioned, and a quite small fraction are hostile.

Here is a video that a group of chemtrails folks took and posted when they came 
to talk with me. You get a good sense of the range concerns:

http://www.youtube.com/watch?v=_SFVYRZPXLs

The Chemtrails believers are one extreme of a continuum. Here is some text on 
the topic from a short book I am writing:

Critiques of geoengineering arise from diverse world views, indeed some of the 
strongest critical voices come from diametrically opposed ends of the political 
spectrum. Passions run very hot.  To cite a vivid personal example, I have had 
one death threat that was serious enough to warrant a call to the police, and 
received many outraged comments by colleagues whom I respect.  The most extreme 
critiques (and the death threat) come from people who are convinced by the 
chemtrails conspiracy theory which holds that the US government is deliberately 
spraying its citizens with toxins from aircraft. Believers claim that metals 
such as aluminum and barium are sprayed from commercial aircraft for purposes 
that are alleged to range from mass culling the human population to mind 
control. These views are wildly held, one sixth of respondents in a large 
public survey we ran in Canada, Brittan and the US believed that is was 
partially or completely true that The government has a secret program that 
uses airplanes to put harmful chemicals into the air.

Our poll found that people are more likely to oppose geoengineering if they are 
skeptical of government authority and self-identify with right end of the 
political spectrum. While chemtrails believers are clearly an extreme, they are 
a coherent part of a continuum that includes a much larger group who believe 
that climate risks are being exaggerated by the environmental left as an excuse 
to justify further extension of state power at the expense of individual 
freedoms. To overstate it, this view sees geoengineering as a tool used by a 
technocratic, transnational, and godless elite who have concocted both the 
climate threat and the geoengineering response as a means to extend their power.




From: geoengineering@googlegroups.com [mailto:geoengineering@googlegroups.com] 
On Behalf Of Ken Caldeira
Sent: Saturday, February 11, 2012 6:16 PM
To: rob...@envsci.rutgers.edu
Cc: geoengineering
Subject: Re: [geo] Fwd: Better brush up on your lies

I think it is not helpful to think of them as enemies. I see these people as 
victims of past government lies and, in many cases, their own mental 
instability.

These people have been living under a government that has started secret wars, 
has secretly kidnapped and tortured people, and so on. They have lived under a 
government that has lied to them repeatedly.

These people have no technical background to distinguish ordinary jet contrails 
from paranoiac visions of massive government conspiracies.  They see jet trails 
becoming more numerous over the decades and are too innumerate to associate 
this increase with increase in jet travel.

They have been taught that they cannot trust government statements, they 
certainly don't trust scientists, and now they are left with no source that 
they can trust (other than their like-minded fellow conspiracy theorists.)

I prefer to see these ChemTrails folks as victims, both of past government lies 
and, in many cases I suspect, of some degree of mental illness.

So, let's not look at them as enemies, but as people who need help.

On Sat, Feb 11, 2012 at 3:22 PM, Alan Robock 
rob...@envsci.rutgers.edumailto:rob...@envsci.rutgers.edu wrote:
For you all to get the flavor of some of our enemies.

For some reason, a discussion I had with a chemtrails demonstration outside the 
AAAS meeting in San Diego two years ago, and which was posted to YouTube then, 
has reappeared on a website, and this is in reaction to that.

Of course, the person who sent this did not sign it.




Alan



[On sabbatical for current academic year.  The best way to contact me

is by email, rob...@envsci.rutgers.edumailto:rob...@envsci.rutgers.edu, or at 
732-881-1610tel:732-881-1610 (cell).]



Alan Robock, Professor II (Distinguished Professor)

  Editor, Reviews of Geophysics

  Director, Meteorology Undergraduate Program

  Associate Director, Center for Environmental Prediction

Department of Environmental SciencesPhone: +1-732-932-9800 
x6222tel:%2B1-732-932-9800%20x6222

Rutgers University  Fax: 
+1-732-932-8644tel:%2B1-732-932-8644

14 College Farm Road   E-mail: 
rob...@envsci.rutgers.edumailto:rob...@envsci.rutgers.edu

New Brunswick, NJ 08901-8551  USA  
http://envsci.rutgers.edu/~robockhttp://envsci.rutgers.edu/%7Erobock


 Original Message 
Subject:

Better brush up on your lies

Date:

Sat, 11 Feb 2012 06:35:28 -0800 (PST)

From:

winsom88 

RE: [geo] Re: Direct Air Capture Summit

2012-02-02 Thread David Keith
Charlie

I doubt this will happen.

The correlation between costs of real hardware and what's citable is very week.

I could find you academic cites for the cost of solar, nuclear or CCS that 
varied by an order of magnitude, but that does not mean the actual cost right 
now in a real location under actual economic conditions is that uncertain.

The bottom line is that the academic literature is a poor place to go for 
industrial costs of anything (except well studied commodities). 

Take solar, for example, I feel like I have a good sense of costs, but that's 
from lots of interaction with top consultants to the business and from some 
presentations, e.g., form Bloomberg Energy Finance, that are not on the web.

Air capture is ***much***less developed. There are a only handful of serious 
development efforts and they are private. I run one of them and we are spending 
well over $1m per year to do the engineering and costing of the processes we 
are working on. 

I don't think you will see a robust consensus on cost emerge for at least a 
decade. Particularly given that the way the early dialog as played out has made 
the situation so combative that cost information is obscured by folks loudly 
taking extreme positions.

I hope you are still juggling. I am teaching my kids.

Ciao,
David




-Original Message-
From: geoengineering@googlegroups.com [mailto:geoengineering@googlegroups.com] 
On Behalf Of Charlie Zender
Sent: Thursday, February 02, 2012 10:58 AM
To: geoengineering
Subject: [geo] Re: Direct Air Capture Summit

This DACS conference will be a watershed event if it succeeds in significantly 
narrowing the consensus range of DAC cost from $10--1000
tCO2 to something, well, narrower. Should that occur, I hope the organizers 
will publish a conference report in a mainstream academic journal like Eos so 
1. the wider community takes notice, and 2. we can cite it. Looks likely the 
number will appear in the Economist first, though.
Charlie

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RE: [geo] New CO2 Sucker Could Help Clear the Air

2012-01-12 Thread David Keith
The answer to Ken's rhetorical question is a qualified yes, if you ignore 
kinetics and assume you are looking only at the CO2 capture, desorption, 
clean-up and compression as he described then you can do it for pennies a kg of 
CO2 which is pennies per kWh. It's a yes because posed this way, ignoring 
kinetics and the capital and energy cost of the absorber this is the core of 
the standard engineering case for post-combustion CCS that has been analyzed 
endlessly for 20 years and for which there is lots of relevant commercial 
hardware.
The qualification is around details of this particular material, but there are 
other solid and liquid systems that do this.
For air capture it's harder because one cannot ignore the kinetics of uptake 
and the capital cost of the absorber structure.
There is not much CO2 in the air so the contacting structure (the thing that 
actually gets CO2 from the air) must be very cheap. Here are some order of 
magnitude numbers:
1. You can't afford to move the air faster than a few m/s though the device 
(100 Pa= 6.1 kJ/mol-C= 13 m/s)
2. At that air flow, even if you get all the CO2 you are getting no more than 
of order 10 tCO2 m-2 yr-1.
3. Assume it is 10 tCO2 m-2 yr-1 and you don't want to pay more than 50 $/tCO2 
for the amortized cost of the structure. Then the cost per square meter of 
inlet area must be less than 3 $k. (At 15% overall capital charge factor $3000 
m-2 is $45 m-2 yr-1 which you then divide by the 10 tCO2 and round). This is 
hard. Large cooling towers are about $2000 m-2.
4. The amount of absorbing surface you need behind each square meter of inlet 
is depends on the kinetics of uptake, but at a mass transfer coefficient of 1 
mm/sec one needs of order 500 m2 of surface area behind each 1 m2 of inlet.
5. For us a Carbon Engineering, using plastic packing it easy to meet this cost 
criteria as they cost 1$ per m2 of surface area. For our system packing cost is 
only a small fraction of contactor cost and a very small fraction of overall 
turn-key plant cost.
6. In order for a solid system to compete it must either have a much faster 
mass transfer coefficient or by roughly as cheap; and for a solid one must 
contrive a way to temperature or humidity cycle the whole solid structure 
cheaply and without significant air leaks. (Or find a way to gather the 
solids...).
You can see some of our views about solid vs liquid systems at answer QA #8 at 
http://www.carbonengineering.com/wp-content/uploads/2011/04/CarbonEngineering-AirCaptureFAQ.pdf.
Of course, the disadvantage of a liquid system is regeneration and management 
of liquid loss.
The problems for solids are (a) getting fast uptake kinetics, (b) cycling given 
that the whole structure must be cycled either humidity swing or thermal swing, 
and (c) sorbent lifetime given that all the fancy solid must last for order a 
decade in air that contains contaminants such as particulates, trace gases and 
larger debris of all types.
Bottom line: this looks like a real advance but without data on kinetics and 
long-term performance one can't judge how useful it is for air capture.
In the near term we are reasonably confident that our liquid system will win 
for many large-scale air capture applications, but over the long run it's much 
harder to say what will happen.


From: geoengineering@googlegroups.com [mailto:geoengineering@googlegroups.com] 
On Behalf Of Ken Caldeira
Sent: Wednesday, January 11, 2012 1:47 PM
To: r...@llnl.gov
Cc: zen...@uci.edu; geoengineering
Subject: Re: [geo] New CO2 Sucker Could Help Clear the Air

Note that there is an error of 10^6 in the article, as it says 1.72 nmol when 
the underlying article (attached) says mmol.

Here is my little order-of-magnitude analysis:

At 1.72 mmol per gram of material, to process 1 ton of CO2, we have would need 
~13 tons of polyamine.

The 1 g of material absorbs at 25 C needs to be heated to 85 C for three hours 
to give off the CO2, so this is a 60 C swing. Of course, one thing conventional 
power plants have is a lot of waste heat. Once it gives off the CO2, it gives 
it off into some gas, so you still need to figure out how to separate the CO2 
from this gas. [Or maybe you make a high vacuum, but how cheap is that? If you 
didn't want to go with a vacuum, what would be the gas that you would have it 
desorb into, in order to make that separation step easy?]

The average CO2 intensity of electricity production is about 615 gCO2/kWh. So 
you would need about 8 kg of material per kWh of electricity.  If the real 
process were to take 3 hours, then you would need about 25 kg of material per 
kW of plant capacity  (or 25,000 tons per GW).

Can you take 8 kg of material (enough for 1 kWh's worth of CO2), have it absorb 
CO2, heat it up and let it desorb into a vacuum or a gas (and if a gas, then 
separate the CO2 from whatever the gas it desorbed into), and then compress and 
bury it underground, for not more than a few pennies per cycle?

Re: [geo] Occupy Wall Street Goes After Geoengineering

2011-10-31 Thread David Keith


- Original Message -
From: Josh Horton [mailto:joshuahorton...@gmail.com]
Sent: Monday, October 31, 2011 03:20 PM
To: geoengineering geoengineering@googlegroups.com
Subject: [geo] Occupy Wall Street Goes After Geoengineering

Hi everyone,

Whatever your views, it was only a matter of time ...

(John Bellamy Foster is editor of the socialist Monthly Review)

http://mrzine.monthlyreview.org/2011/foster291011.html


Capitalism and Environmental Catastrophe
by John Bellamy Foster

John Bellamy Foster and Fred Magdoff at Occupy Wall Street.  Photo by
Carrie Ann Naumoff
This is a reconstruction from notes of a talk delivered at a teach-in
on The Capitalist Crisis and the Environment organized by the
Education and Empowerment Working Group, Occupy Wall Street, Zuccotti
Park (Liberty Plaza), New York, October 23, 2011.  It was based on a
talk delivered the night before at the Brecht Forum.  Fred Magdoff
also spoke on both occasions.

The Occupy Wall Street movement arose in response to the economic
crisis of capitalism, and the way in which the costs of this were
imposed on the 99 percent rather than the 1 percent.  But the highest
expression of the capitalist threat, as Naomi Klein has said, is its
destruction of the planetary environment.  So it is imperative that we
critique that as well.1

I would like to start by pointing to the seriousness of our current
environmental problem and then turn to the question of how this
relates to capitalism.  Only then will we be in a position to talk
realistically about what we need to do to stave off or lessen
catastrophe.

How bad is the environmental crisis?  You have all heard about the
dangers of climate change due to the emission of carbon dioxide and
other greenhouse gases into the atmosphere -- trapping more heat on
earth.  You are undoubtedly aware that global warming threatens the
very future of the humanity, along with the existence of innumerable
other species.  Indeed, James Hansen, the leading climatologist in
this country, has gone so far as to say this may be our last chance
to save humanity.2

But climate change is only part of the overall environmental problem.
Scientists, led by the Stockholm Resilience Centre, have recently
indicated that we have crossed, or are near to crossing, nine
planetary boundaries (defined in terms of sustaining the
environmental conditions of the Holocene epoch in which civilization
developed over the last 12,000 years): climate change, species
extinction, the disruption of the nitrogen-phosphorus cycles, ocean
acidification, ozone depletion, freshwater usage, land cover change,
(less certainly) aerosol loading, and chemical use.  Each of these
rifts in planetary boundaries constitutes an actual or potential
global ecological catastrophe.  Indeed, in three cases -- climate
change, species extinction, and the disruption of the nitrogen cycle
-- we have already crossed planetary boundaries and are currently
experiencing catastrophic effects.  We are now in the period of what
scientists call the sixth extinction, the greatest mass extinction
in 65 million years, since the time of the dinosaurs; only this time
the mass extinction arises from the actions of one particular species
-- human beings.  Our disruption of the nitrogen cycle is a major
factor in the growth of dead zones in coastal waters.  Ocean
acidification is often called the evil twin of climate change, since
it too arises from carbon dioxide emissions, and by negatively
impacting the oceans it threatens planetary disruption on an equal
(perhaps even greater) scale.  The decreased availability of
freshwater globally is emerging as an environmental crisis of
horrendous proportions.3

All of this may seem completely overwhelming.  How are we to cope with
all of these global ecological crises/catastrophes, threatening us at
every turn?  Here it is important to grasp that all of these rifts in
the planetary system derive from processes associated with our global
production system, namely capitalism.  If we are prepared to carry out
a radical transformation of our system of production -- to move away
from business as usual -- then there is still time to turn things
around; though the remaining time in which to act is rapidly running
out.

Let's talk about climate change, remembering that this is only one
part of the global environmental crisis, though certainly the most
urgent at present.  Climate science currently suggests that if we burn
only half of the world's proven, economically accessible reserves of
oil, gas, and coal, the resulting carbon emissions will almost
certainly raise global temperatures by 2° C (3.6° F), bringing us to
what is increasingly regarded as an irreversible tipping point --
after which it appears impossible to return to the preindustrial
(Holocene) climate that nourished human civilization.  At that point
various irrevocable changes (such as the melting of Arctic sea ice and
the ice sheets of Greenland and Antarctica, and the release of 

RE: [geo] White roof snag

2011-10-28 Thread David Keith
Greg et al

There are a number of reasons why white roofs might cause heating that are well 
explained in the paper. Among them local suppression of convection and the 
correlation between where the roofs are and absorbing dust particles. The roofs 
we plan to whiten tend to be in places with dirty air, and so the problem of 
absorption is much more pronounced than if we scattered the whitening randomly 
over the planet.

Your analogy to large-scale albedo changes is false because both the 
interaction with convection and the correlation with dirty air are not present 
in that case. 

I think it will take more papers to really nail this down but there's nothing 
impossible about this result and at a glance the paper seems sensible and 
serious.

Http://www.stanford.edu/group/efmh/jacobson/Articles/Others/HeatIsland+WhiteRfs0911.pdf

David


-Original Message-
From: geoengineering@googlegroups.com [mailto:geoengineering@googlegroups.com] 
On Behalf Of Rau, Greg
Sent: Friday, October 28, 2011 10:40 AM
To: s.sal...@ed.ac.uk; geoengineering@googlegroups.com
Subject: RE: [geo] White roof snag

A worldwide conversion to white roofs, they found, could actually warm the 
Earth slightly due a complex domino effect. Although white surfaces are cooler, 
the increased sunlight they reflect back into the atmosphere by can increase 
absorption of light by dark pollutants such as black carbon, which increases 
heating. 

So by analogy, increased snow/ice cover would actually warm the Earth 
slightly ?  I don't think so, but please clue me in. - Greg

 

From: geoengineering@googlegroups.com [geoengineering@googlegroups.com] On 
Behalf Of Stephen Salter [s.sal...@ed.ac.uk]
Sent: Friday, October 28, 2011 4:22 AM
To: geoengineering@googlegroups.com
Subject: [geo] White roof snag

Hi All

See

http://www.guardian.co.uk/environment/2011/oct/27/white-roofs-global-warming

and

Jacobson, M.,  Ten Hoeve, J. (2011). Effects of Urban Surfaces and White Roofs 
on Global and Regional Climate. Journal of Climate DOI: 
10.1175/JCLI-D-11-00032.1http://dx.doi.org/10.1175/JCLI-D-11-00032.1

Stephen

Emeritus Professor of Engineering Design Institute for Energy Systems School of 
Engineering Mayfield Road University of Edinburgh EH9  3JL Scotland Tel +44 131 
650 5704 Mobile 07795 203 195 
www.see.ed.ac.uk/~shshttp://www.see.ed.ac.uk/~shs




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RE: [geo] Home critique of Keith mercer paper

2011-10-24 Thread David Keith
Andrew

I am not a geoengineer, whatever that would mean.

I am someone who has work for 20 years on a variety of climate and energy 
problems, including work on such basic stuff has measuring the rate of climate 
change. It is relevant to the work at hand that I have worked with some of the 
leading experts in assessing public opinion of emerging technologies, and that 
we used these techniques this study.

ETC/Home evidently lacks anything substantive to say about why our study is 
incorrect and dislikes the conclusion so they cry bias.

This is exactly what happens when I talk to the press and say that we cannot 
keep adding carbon to the atmosphere if we want a stable climate and that as a 
consequence they should shut down the oil industry. The oil industry 
representatives in Calgary cry bias arguing I have an interest in promoting 
climate change.

Bias is always an easy claim you don't like the conclusions.

ETC/Home argues that I am biased because I do commercial work on air capture 
and they assert that I support commercial work on SRM. In fact I oppose 
commercial work on SRM and would like to see such work prohibited where 
feasible. For example, I have advocated mechanisms to eliminate the possibility 
of patenting SRM technologies.

The bias claim is doubly odd because if SRM was accepted as being a cheap and 
easy fix then there would be no market for CO2 scrubbing which is expensive. 
Therefore if I am biased in promoting SRM, I am biased against my self-interest.

The other authors and reviewers of this paper have no obvious interest in 
promoting SRM and have an obvious self-interest in avoiding the damage to their 
careers by engaging in deliberately biased studies.

We make no claims to have asked questions about SPICE. This claim by ETC is 
based solely on the release that was written by the PR person at ERL. As is a 
matter of public record (google it) I think the SPICE hose test is a serious 
mistake, so it is certainly not in my interest to promote it. I would like to 
see it canceled. If it succeeds it's only benefit of will be to make SRM 
cheaper which is precisely what we do not need. Any research on SRM in the 
atmosphere it should be focused on understanding and minimizing environmental 
risks.

ETC/Home have an obvious bias in that they are an advocacy organization with a 
strong position to defend. Whatever the merits of this position, it simply 
their job to say whatever is necessary to discredit information that seems to 
point in a direction they do not like. This is a group that has talked about 
chemtrails on their webpage.

David





From: geoengineering@googlegroups.com [mailto:geoengineering@googlegroups.com] 
On Behalf Of Andrew Lockley
Sent: Monday, October 24, 2011 4:42 PM
To: geoengineering
Subject: [geo] Home critique of Keith mercer paper


A leading Geoengineer has today published a public opinion survey which is 
being reported as showing broad public support of geoengineering research. 
Suspicious? The reality of course is nothing so clear. The paper is authored by 
geoengineering advocate (and commercial geoengineer) David Keith and 2 other 
authors - one of whom is Keith's Doctoral student. While the press release 
claims as its headline that 72% of those interviewed support geoengineering 
research and that this has important implications for the SPICE project (trojan 
hose experiment) - actually:

- the questions were only about SRM (not 'geoengineering') - the question 
actually never asked about 'research' and certainly not about experimentation 
or SPICE (it asked only whether scientists should 'study' SRM) - Some of the 
strongest opinions expressed by those interviewed were very critical of SRM but 
these weren't mentioned in the press release even though there was stronger 
support for these critical opinions than the 'headline'. - The opinions of over 
200 people were excluded from the study at the discretion of 2 of the 
researchers on the basis that those people had read about SRM online. - When 
asked, 38% of those who responded to the survey identified the description of 
SRM given to them as biased in favour of SRM. Only about 2% thought it was 
biased against.

Here is a report in The Guardian about the survey: 
http://www.guardian.co.uk/environment/2011/oct/24/geoengineering-survey-public-support?
 newsfeed=true
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RE: [geo] Wind and wave energies are not renewable after all

2011-07-12 Thread David Keith
Mike  Bala

A few answers:

First there is almost no link to geo here so we should probably take this off 
this list. The only (weak link) is weather control, see: 
http://www.atmos-chem-phys.org/10/769/2010/acp-10-769-2010.html

1. Bala said Generation of wind energy would increase the KE dissipation rate 
but this is not an external forcing to the climate system. And The current KE 
dissipation rate is about 2 watts/m^2. Over land, this translates to about 300 
TW. Suppose wind farms extract 150 TW (which may be impractical), the 
dissipation rate over land will increase to 3 Wm^2. Don't you think the KE (or 
available PE) generation rate in the atmosphere would correspondingly increase? 
Of course these would be large regional climate changes.

Answer: As the surface drag is increased the total dissipation does not change 
much. That is, as you increase the KE sink in some locations with wind turbines 
the dissipation decreases elsewhere keeping total about constant. See Figure 2 
of our 2004 PNAS where we tried this. This is what one would expect because 
dissipation of KE must balance its creation from APE (see pexoto and ort or my 
encyclopedia article cited below for an overview of atmo energetics). Going a 
bit deeper one might think that with more to push against the APE generation 
rate would go up and the atmo heat engine get more efficient, Kerry Emanuel 
have suggested to me that this should not be true because of a maximum entropy 
principle that I do not fully understand.

Bottom line: very likely Bala's assumption is wrong.

2. Bala said: I agree there would be local and regional climate changes but 
there should be no global mean warming. Right?

Answer: mostly. One can see either warming or cooling depending on where the 
wind drag is applied. The point is that (a) climate changes due to drag are 
non-local, and (b) they can be large.

3. Mike asked about the Jacobsen paper that says no effect.

Answer: I think this paper is just wrong. If it were true I could violate the 
first law by extracting power without altering KE and then using that power to 
increase APE generating infinite power with no input. Nice trick.  There are 
now about 5 studies that confirm the broad results in our 2004 paper. The 
Jacobsen paper is an outlier. I expect a convincing critique will be published 
in the next few years.

Yours,
David




From: geoengineering@googlegroups.com [mailto:geoengineering@googlegroups.com] 
On Behalf Of Mike MacCracken
Sent: Tuesday, July 12, 2011 6:22 AM
To: Govindasamy Bala; David Keith; Ken Caldeira
Cc: Geoengineering
Subject: Re: [geo] Wind and wave energies are not renewable after all

Dear David--I was going to ask a similar question to Bala's-as this has 
actually been an ongoing argument in some circles of the energy community, with 
a scientific study by a Royal Society lead physicist in their energy analysis 
talking about a limit based on extracting a share of the existing atmospheric 
KE and Mark Jacobson at Stanford saying there is plenty of KE as it will be 
restored.

It seems to me that the KE pulled out will be replaced-if not, the atmosphere 
would eventually not be moving and so a huge equator-pole temperature gradient 
would build up. With solar energy concentrated at the low latitudes and IR loss 
in excess at high latitudes, the atmosphere will be seeking balance; take some 
energy out and the atmosphere will try to restore it, rather like what happens 
when one puts a rock in a stream, maybe with a bit different flow, but I would 
not think significantly less KE. Right?

Mike



On 7/12/11 7:25 AM, Govindasamy Bala bala@gmail.com wrote:
Hi David,

Couple of questions.
Generation of wind energy would increase the KE dissipation rate but this is 
not an external forcing to the climate system. I agree there would be local and 
regional climate changes but there should be no global mean warming. Right?

The current KE dissipation rate is about 2 watts/m^2. Over land, this 
translates to about 300 TW. Suppose wind farms extract 150 TW (which may be 
impractical), the dissipation rate over land will increase to 3 Wm^2. Don't you 
think the KE (or available PE) generation rate in the atmosphere would 
correspondingly increase? Of course these would be large regional climate 
changes.

Bala

On Tue, Jul 12, 2011 at 8:37 AM, David Keith ke...@ucalgary.ca wrote:
Responding to a VERY old thread on wind power:

The only link to geoengineering here is that there is a possibility of 
manipulating wind turbine drag for weather control, see:

At 10's TW scale extraction of wind does begin to be constrained by the 
generation of kinetic energy. I led the a joint NCAR-GFDL group that published 
the first paper on this topic see:
David W. Keith et al, The influence of large-scale wind-power on global 
climate. Proceedings of the National Academy of Sciences, 101, p. 16115-16120.
http://people.ucalgary.ca/~keith/papers/66.Keith.2004.WindAndClimate.e.pdf 
http

RE: [geo] HOME/ETC Group Targets IPCC: Data on public perception

2011-07-11 Thread David Keith
Folks

Earlier comments on this thread contained lots of speculation about what people 
think about SRM/geo.

We recently submitted a paper that has some of the first results from a 
high-quality surveys of public perception. (Where for a survey, 
high-quality=that is big numbers, good demographic sampling, and well tested 
questions.) 

The paper is at http://people.ucalgary.ca/~keith/Preprints.html. You need a 
username  password which you can get (quickly) from the Hollie Roberts see 
email link on the page (and I don't change it). 

Yours,
David


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RE: [geo] Wind and wave energies are not renewable after all

2011-07-11 Thread David Keith
Responding to a VERY old thread on wind power:

The only link to geoengineering here is that there is a possibility of 
manipulating wind turbine drag for weather control, see:

At 10's TW scale extraction of wind does begin to be constrained by the 
generation of kinetic energy. I led the a joint NCAR-GFDL group that published 
the first paper on this topic see:
David W. Keith et al, The influence of large-scale wind-power on global 
climate. Proceedings of the National Academy of Sciences, 101, p. 16115-16120.
http://people.ucalgary.ca/~keith/papers/66.Keith.2004.WindAndClimate.e.pdf

See 
http://people.ucalgary.ca/~keith/papers/94.Kirk-Davidoff.SurfaceRoughnessJAS.p.pdf
 for a paper that says a bit about why it happens.

The following web page gives and overview but it's now out of date: 
http://people.ucalgary.ca/~keith/wind.html

Alvia's comment that about kinetic energy, i.e. the motion of molecules, 
confuses the physics. Kinetic energy is macroscopic velocity, random motion of 
molecules is just heat. It is true that large scale production and dissipation 
of kinetic energy must balance, have a look at Peixoto and Oort's the Physics 
of Climate or a short encyclopedia article I one wrote on atmospheric 
energetics: 
http://people.ucalgary.ca/~keith/papers/15.Keith.1996.Energetics.s.pdf

Bottom lines:

1. Commonly cited estimates for global wind power potential are too large. On 
cannot get to 100 TW in any practical scheme I know about.

2. At even a few TW large scale climate effects will begin to be important. 
But, this does not say we should not make a few TW of wind, just that--like any 
energy technology-there are tradeoffs.

David

From: geoengineering@googlegroups.com [mailto:geoengineering@googlegroups.com] 
On Behalf Of Nando
Sent: Saturday, April 02, 2011 8:25 AM
To: agask...@nc.rr.com
Cc: andrew.lock...@gmail.com; geoengineering
Subject: Re: [geo] Wind and wave energies are not renewable after all

My reading of the article suggested that the authors of the study were 
principally claiming that wind has an impact on climate, so it is already being 
used. What wasn't clear from the article was what type of impact reducing the 
energy level of winds all over the globe through the prolific use of wind 
turbines might have. In a warming world, I understand we should expect stronger 
winds. On a simplistic generalized level that might not be relevant to local 
climate, slowing those stronger winds down might have an ameliorating effect on 
climate change. Hence the claim that The magnitude of the changes was 
comparable to the changes to the climate caused by doubling atmospheric 
concentrations of carbon dioxide might not be as bad as it is made to seem.

As usually, I'm grasping at straws, but as a layman, that's what stood out for 
me.

Nando
On Sat, Apr 2, 2011 at 3:15 PM, Alvia Gaskill 
agask...@nc.rr.commailto:agask...@nc.rr.com wrote:
Wind and wave energy are the result of the conversion of solar energy into 
kinetic energy, i.e. the motion of molecules.  Once converted into kinetic 
energy it's a use it or lose it proposition.  Extracting kinetic energy from 
the atmosphere or the ocean doesn't mean it won't be replaced by more energy 
from sunlight.  Planting more trees will also intercept winds, albeit without 
the electricity generation.  Who funded this research?  The same people who 
want to prevent contact with alien civilizations?  I note that the Royal 
Society was also a party to that one too.  Note to Royal Society.  When you 
actually find something under the bed I should be afraid of, wake me up.
- Original Message -
From: Andrew Lockleymailto:and...@andrewlockley.com
To: geoengineeringmailto:geoengineering@googlegroups.com
Sent: Friday, April 01, 2011 8:10
Subject: [geo] Wind and wave energies are not renewable after all

Wind and wave energies are not renewable after all
* 30 March 2011 by Mark 
Buchananhttp://www.newscientist.com/search?rbauthors=Mark+Buchanan
* Magazine issue 2806http://www.newscientist.com/issue/2806. 
Subscribe and savehttp://www.newscientist.com/subscribe?promcode=nsarttop
* For similar stories, visit the Energy and 
Fuelshttp://www.newscientist.com/topic/energy-fuels and Climate 
Changehttp://www.newscientist.com/topic/climate-change Topic Guides

Editorial: The sun is our only truly renewable energy 
sourcehttp://www.newscientist.com/article/mg21028062.500-the-sun-is-our-only-truly-renewable-energy-source.html

Build enough wind farms to replace fossil fuels and we could do as much damage 
to the climate as greenhouse global warming

WITNESS a howling gale or an ocean storm, and it's hard to believe that humans 
could make a dent in the awesome natural forces that created them. Yet that is 
the provocative suggestion of one physicist who has done the sums.

He concludes that it is a mistake to assume that energy sources like wind and 
waves are truly renewable. Build enough wind farms to replace fossil fuels, he 

RE: [geo] Cost of Air Capture and the APS report

2011-06-21 Thread David Keith
Of course it's not only an emergency strategy.

Each group that has begun to think about it seriously has realized that.

I said just this to the group in Lima an hour ago.

David

From: Alvia Gaskill [mailto:agask...@nc.rr.com]
Sent: Tuesday, June 21, 2011 3:07 PM
To: soco...@princeton.edu; rongretlar...@comcast.net
Cc: geoengineering@googlegroups.com; David Keith
Subject: Re: [geo] Cost of Air Capture and the APS report


I leave the Lima group with a final thought. Is SRM only an emergency 
strategy? What are the pros and cons of a continuous ground-bass deployment of 
1 W/m^2 of stratospheric aerosol negative forcing, as an overall helper on the 
margin and as a way of learning about larger deployment?



No, it shouldn't only be considered as an emergency option, a term which has 
never been adequately defined anyway and tends to be used as a defense against 
the media and the opponents of geoengineering by those working in the field who 
can't or don't want to pardon the expression, take the heat.



 Paul Crutzen included use of stratospheric aerosols at about this level of 
negative forcing to replace the loss of tropospheric sulfate from pollution 
controls and others have made similar proposals (including me).  To get to some 
kind of full-scale offset of AGW forcing (back to pre-industrial from today or 
some future date) you have to pass through 1 W/m2 anyway.  Plus, a slowdown of 
warming now means less ice melted that we can't replace in the future (given 
what we know about how difficult that will be).   This applies to cloud 
brightening as well or some other technology that could achieve the same 
impact.  But i also note that to get to 1 W/m2 you have to get through 0.1 and 
0.2 and 0.3, etc.  You have to start somewhere.
- Original Message -
From: Robert Socolowmailto:soco...@princeton.edu
To: rongretlar...@comcast.netmailto:rongretlar...@comcast.net
Cc: geoengineering@googlegroups.commailto:geoengineering@googlegroups.com ; 
ke...@ucalgary.camailto:ke...@ucalgary.ca
Sent: Tuesday, June 21, 2011 2:57
Subject: RE: [geo] Cost of Air Capture and the APS report

Ron, Ken, and others:

Given that the Lima meeting is in its middle day today, let me push everything 
aside to write answers to Ron's questions. I am speaking only for myself.


1.   Yes, there is only one change, aside from formatting, in the June 1 
version of the APS report. We say so on the second page of the preface. As we 
were issuing the unformatted version at the end of April, David Keith 
identified a clear mistake in our report, involving the pressure drop per meter 
for a specific packing material, which we had carried forward from a 2006 
paper. Fortunately, one member of our committee, Marco Mazzotti, was an author 
of that paper. With one of his co-authors, he updated his earlier work with new 
information from the manufacturer of the packing, additionally found an error 
in his earlier analysis, followed a hunch that there was an easy fix for us by 
substituting one packing for another, and we buttoned this up. The new packing 
is cheaper, but we verified that our initial cost estimate for packing had been 
so conservative that the new packing actually fit the assumed price better. I 
am aware at this time of no outright error in our report. People may find some, 
and if they do I hope they will tell me about them.



2.   Item a. In my view, the experts (specifically Keith, Lackner, and 
Eisenberger) were given adequate time to interact with us. Our project took two 
years. We established groundrules at the front end that there would be an 
arms-length relationship and (confirmed more than once) that as a matter of 
policy we would not learn confidential information. All three presented to us 
at our kick-off meeting in March 2009, reviewed a draft (along with almost 20 
others) in April 2010, and communicated repeatedly with us. I had the personal 
goal of being sure that the key ideas in their work were understood by our 
committee and commented upon in our report. Nonetheless, none of the three of 
them is happy with the result. One comment all three would make is that they 
would have done the study differently. They would have asked what air capture 
could cost if one were to assume success in the presence of risk; our committee 
felt that in the absence of reviewable published data, this was an illegitimate 
task. We decided to include one cost estimate based on a benchmark design, 
resulting in a system whose cost is probably quite a lot higher than $600/tCO2, 
and in the process, by careful attention to methodology, the reader can learn 
how to think about costs. Personally, I now appreciate (and the reader will too 
who works through the calculation) that the most underestimated cost factor is 
the pressure drop as air moves through the contactor, which enters not only as 
a an energy cost but also through its impact on net carbon, even for largely 
decarbonized power. All three experts

[geo] Cost of Air Capture and the APS report

2011-06-20 Thread David Keith
Several recent posts have referred to the American Physical Society's report on 
Air Capture.

We posted a critique of the report and in turn the APS released an updated 
version that-using a post-facto kluge-addressed two of the errors that had 
identified.

The our comments are posted on 
www.carbonengineering.comhttp://www.carbonengineering.com the website of our 
Air Capture startup company, the deep link is here: 
http://www.carbonengineering.com/wp-content/uploads/2011/05/CE_APS_DAC_Comments.pdf.

We at Carbon Engineering are self-interested. Of course! But that cuts both 
ways. We have a huge incentive do to quality engineering that can be brought to 
market and not to waste our time on stuff that does not make sense.

Speaking for myself, I have opportunities to do commercial work on both AC and 
on biomass with capture (BECCS). And I have access to high quality proprietary 
engineering and economic analysis of both. If I thought that BECCS was much 
cheaper than AC then I would not be working on AC.

David






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RE: IPCC on geo-engineering Re: [geo] geo eng and new Friends of the Earth EWNI report urges very deep and rapid emission cuts

2011-01-04 Thread David Keith
Bhaskar

I don't speak for the IPCC, I am just helping organize the meeting. So are 
several other people on this distribution list. 

The following speculation not a position statement: Given that this is the 
IPCC, and given that it is a coordinating meeting between all three working 
groups, I think there's little danger that the focus will be narrow. However 
exactly the taxonomy is divided, I would guess we will end up with an expansive 
coverage of topics typically called geoengineering. Given there are three 
working groups, the review very likely cover science, environmental impacts, 
and social science issues including issues of governance, distributive justice, 
economics and public perception (one could probably get a decent sense of what 
the coverage might be in this area from looking at previous WG III reports). 

Yours,
D



-Original Message-
From: geoengineering@googlegroups.com [mailto:geoengineer...@googlegroups.com] 
On Behalf Of M V Bhaskar
Sent: Tuesday, January 04, 2011 5:33 AM
To: geoengineering
Subject: Re: IPCC on geo-engineering Re: [geo] geo eng and new Friends of the 
Earth EWNI report urges very deep and rapid emission cuts

Dr Keith

Glad to know you are on the Organising committee for the IPCC WG meetings in 
Peru.

IPCC website says -
Current discussions that suggest geoengineering as an option to support 
climate mitigation efforts remain rather abstract and lack comprehensive risk 
assessments that take into account possible adverse impacts over short and 
longer time frames. Major uncertainties exist regarding the effects of these 
techniques on the physical climate system and on biogeochemical cycles, their 
possible impacts on human and natural systems, and their effectiveness and 
costs. 

In the field of Ocean Fertilization we believe that we have addressed many of 
the risks noted above.
We have been causing controlled blooms of Diatoms on a medium scale for the 
past 5 years.
So the costs, benefits, consequences, etc., are know.

How can we put forth our views to the WG at Peru?

best regards

Bhaskar

On Jan 3, 6:33 pm, David Keith ke...@ucalgary.ca wrote:
 I am on the organizing committee for the IPCC interworking group meeting on 
 geoengineering in Peru this summer.

 The possibility of a special report will no doubt be discussed at some length 
 at that meeting.

 My views are pretty well aligned with Ken's here. There are lots of summary 
 reports written in more in the works, what is lacking is sufficient serious 
 analysis of the various methods, their potential, risks and uncertainties.

 -D


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RE: [geo] Carbon sequestration workshop Sep 9-10, Heinz Center, Washington DC

2010-09-15 Thread David Keith
Marty,

Thanks for this gracious response.

Sometimes, not often, I miss being back in physics.

Cheers,
D

From: Marty Hoffert [mailto:marty.hoff...@nyu.edu]
Sent: Wednesday, September 15, 2010 7:11 AM
To: David Keith
Cc: z...@atmos.umd.edu; geoengineering@googlegroups.com; James Rhodes
Subject: Re: [geo] Carbon sequestration workshop Sep 9-10, Heinz Center, 
Washington DC

I agree with David that whether to bury or to burn depends on details like 
whether you can burn the biomass AND bury its CO2, and whether you are looking 
at methane or coal as the alternate fuel for generating electricity.

A big problem is that we have too few pilot plants measuring actual performance 
versus idealized limits in parameter space. This is a problem for all alternate 
energy sources. People get into huge arguments over these numbers and come to 
different conclusions about a technology's viability.

I like to think we engineer/applied physics types are ethically compelled to 
abandon our beautiful theories in the face of ugly facts -- something our 
social science colleagues aren't quite as obsessed about. The reason I 
circulated that paper from climatic change was to stimulate quantitative 
discussion  if it did I'm happy.


Marty Hoffert

Sent from my iPhone

On Sep 14, 2010, at 8:42 PM, David Keith 
ke...@ucalgary.camailto:ke...@ucalgary.ca wrote:

Andrew et al



A few comments on this thread.



Ning Zeng has it right, statements that burying beats burning in all (or even 
most) cases are not supported by the evidence.



This is a case with the details and circumstances matter.



If you have wet waste near the Mississippi and the alternative is combustion of 
the waste in a purpose-built biomass to electricity facility (which will be 
small, inefficient, and of high capital costs) then burial wins.



If you have somewhat dry waste near a coal-fired power plant then cofiring wins.



Marty said fundamentally it's better to bury them burn. Marty is smart guy. 
We both have the curse or blessing of physics as a background. But I have to 
say I am mystified how anyone can make any kind of fundamental claim that 
either burial or burning is better. I don't see any evidence for that claim in 
the paper.



Stuart said: All of these arguments were answered last year when the paper 
came out, but apparently you did not digest them then, so I will repeat, 
briefly.  Burning biomass for electricity or making ethanol avoids fossil fuel 
carbon emissions = 30%  of the starting biomass carbon.  Biomass is a poor 
fuel, better to bury it.  Please read the paper.  Or is there something about 
31 that you don’t understand?



I don't think the problem is our failure to understand that 31, nor do I think 
that this style of rhetoric helps settle arguments on complicated topics. In 
this particular case, the 30% depends on a set of assumptions, which in some 
cases might be true, in some cases burial is better than burning. However in 
other cases (many) they're not true.



When you do the economic analysis in $/tC terms and finds that things that are 
easy breeze by matter. Example: capital costs. If you have to build a purpose 
built biomass facility than the capital cost will be well north of 2000 $/kWe 
and it may look big compared to the equivalent cost of building the 
infrastructure to do the burial. If, you're talking about retrofitting for 
cofiring then the capex looks 5X smaller. Utilization of capital also matters, 
biomass is a variable resource. One advantage of cofiring is that the capital 
is used all the time, if there's no biomass you just use the coal. Where is 
dedicated biomass systems must stand idle when there's not much biomass, when 
you calculate dollars per ton you have less utilization per unit capital and 
prices go up.



Here's some of our papers that address these points:



47. David W. Keith and James S. Rhodes (2002). Bury, burn or both: A 
two-for-one deal on biomass carbon and energy. Climatic Change, 54: 375-377.

This paper was invited with the paper Marty referred to because that Steve 
Schneider was concerned that the burial paper seem too much like advocacy, and 
wanted to hear another point of view.



95. James S. Rhodes and David W. Keith. (2008). Biomass with Capture: Negative 
Emissions Within social and Environmental Constraints. Climatic Change, 87: 
321-328.

A more general overview of various pathways to negative 
emissions.



64. Allen L. Robinson, James S. Rhodes and David W. Keith (2003). Assessment of 
Potential Carbon Dioxide Reductions due to Biomass-Coal Cofiring in the United 
States. Environmental Science and Technology, 37: 5081-5089.

This paper was an attempt to quantify the potential of cofiring by doing a 
state-by-state match of biomass resources and coal-fired power. There are 
obvious limitations to this analysis, but it will least it was an attempt to go 
beyond gross national averages. It also contains a review of the status cofire

RE: [geo] Carbon sequestration workshop Sep 9-10, Heinz Center, Washington DC

2010-09-14 Thread David Keith
Andrew et al



A few comments on this thread.



Ning Zeng has it right, statements that burying beats burning in all (or even 
most) cases are not supported by the evidence.



This is a case with the details and circumstances matter.



If you have wet waste near the Mississippi and the alternative is combustion of 
the waste in a purpose-built biomass to electricity facility (which will be 
small, inefficient, and of high capital costs) then burial wins.



If you have somewhat dry waste near a coal-fired power plant then cofiring wins.



Marty said fundamentally it's better to bury them burn. Marty is smart guy. 
We both have the curse or blessing of physics as a background. But I have to 
say I am mystified how anyone can make any kind of fundamental claim that 
either burial or burning is better. I don't see any evidence for that claim in 
the paper.



Stuart said: All of these arguments were answered last year when the paper 
came out, but apparently you did not digest them then, so I will repeat, 
briefly.  Burning biomass for electricity or making ethanol avoids fossil fuel 
carbon emissions = 30%  of the starting biomass carbon.  Biomass is a poor 
fuel, better to bury it.  Please read the paper.  Or is there something about 
31 that you don't understand?



I don't think the problem is our failure to understand that 31, nor do I think 
that this style of rhetoric helps settle arguments on complicated topics. In 
this particular case, the 30% depends on a set of assumptions, which in some 
cases might be true, in some cases burial is better than burning. However in 
other cases (many) they're not true.



When you do the economic analysis in $/tC terms and finds that things that are 
easy breeze by matter. Example: capital costs. If you have to build a purpose 
built biomass facility than the capital cost will be well north of 2000 $/kWe 
and it may look big compared to the equivalent cost of building the 
infrastructure to do the burial. If, you're talking about retrofitting for 
cofiring then the capex looks 5X smaller. Utilization of capital also matters, 
biomass is a variable resource. One advantage of cofiring is that the capital 
is used all the time, if there's no biomass you just use the coal. Where is 
dedicated biomass systems must stand idle when there's not much biomass, when 
you calculate dollars per ton you have less utilization per unit capital and 
prices go up.



Here's some of our papers that address these points:



47. David W. Keith and James S. Rhodes (2002). Bury, burn or both: A 
two-for-one deal on biomass carbon and energy. Climatic Change, 54: 375-377.

This paper was invited with the paper Marty referred to because that Steve 
Schneider was concerned that the burial paper seem too much like advocacy, and 
wanted to hear another point of view.



95. James S. Rhodes and David W. Keith. (2008). Biomass with Capture: Negative 
Emissions Within social and Environmental Constraints. Climatic Change, 87: 
321-328.

A more general overview of various pathways to negative 
emissions.



64. Allen L. Robinson, James S. Rhodes and David W. Keith (2003). Assessment of 
Potential Carbon Dioxide Reductions due to Biomass-Coal Cofiring in the United 
States. Environmental Science and Technology, 37: 5081-5089.

This paper was an attempt to quantify the potential of cofiring by doing a 
state-by-state match of biomass resources and coal-fired power. There are 
obvious limitations to this analysis, but it will least it was an attempt to go 
beyond gross national averages. It also contains a review of the status cofire 
technology by Allen Robinson a colleague at CMU who is a combustion expert. 
N.B., this paper has an error in one of the axis labels of the final figure. 
Jamie: if you're reading please double check that we have a corrected version 
up.



126. Jamie Rhodes and David Keith (2009). Biomass co-utilization with 
unconventional fossil fuels to advance energy security and climate policy. 
National Commission on Energy Policy

Finally, things look different again when you consider gasification pathways to 
co-processing. Here the disadvantage of wet biomass is less important. This is 
a report we wrote more recently summarizing these options for a major 
Washington think tank.



All of these papers are available for free download at 
http://people.ucalgary.ca/~keith/Other%20Energy.html.



To sum up, I am not claiming that burial is foolish. It's a good idea that make 
sense under some circumstances. I am claiming that statements to the effect 
that burial is fundamentally or obviously better is advocacy not analysis.



Yours,

David







-Original Message-
From: geoengineering@googlegroups.com [mailto:geoengineer...@googlegroups.com] 
On Behalf Of Ning Zeng
Sent: Monday, September 13, 2010 6:40 AM
To: geoengineering
Subject: Re: [geo] Carbon sequestration workshop Sep 9-10, Heinz Center, 
Washington DC



Dear Andrew and all

[geo] Several papers

2010-09-02 Thread David Keith
 
policy under uncertainty. We find that the quick response allowed by SRM makes 
it important even if it is relatively ineffective at compensating for 
CO2-driven climate change or even if its costs are expected to be large 
compared to traditional mitigation strategies. Finally, we examine the 
implications of uncertainty about the effectiveness of SRM and show that the 
value of reducing this uncertainty can readily exceed several trillion US 
dollars over the next 100 years, providing a strong argument for a research 
program.


David Keith
Canada Research Chair in Energy and the Environment
www.ucalgary.ca/~keithhttp://www.ucalgary.ca/~keith
ke...@ucalgary.camailto:ke...@ucalgary.ca
(403) 220-6154

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RE: [geo] Joe Romm post and comment on attending the Asilomar meeting

2010-03-21 Thread David Keith
Margaret,

The board statement clarifies the goals of CRF. These goals seem admirable and 
entirely appropriate for an organization sponsoring a meeting like Asilomar. 
For my part, they answer the questions central I raised in my correspondence 
with Joe Romm. 

This relieves my concerns about attending the meeting.

Thank you very much for this.

I look forward to seeing you tomorrow. 

Yours,
David


From: geoengineering@googlegroups.com [mailto:geoengineer...@googlegroups.com] 
On Behalf Of Margaret Leinen
Sent: March 21, 2010 1:08 PM
To: Ken Caldeira; geoengineering
Subject: Re: [geo] Joe Romm post and comment on attending the Asilomar meeting

Some have speculated to this group about my motivation and that of the Climate 
Response Fund in sponsoring the upcoming Asilomar International Conference on 
Climate Intervention Technologies.

Recently the Board of Directors of the Climate Response Fund (and I am a member 
of the Board) posted a statement explicitly stating that we will not fund 
climate intervention experiments now or in the future.  The statement also 
addresses other concerns that have been raised in blogs.

The statement is located at:

http://www.climateresponsefund.org/index.php?option=com_contentview=articleid=147Itemid=87

Margaret Leinen
-- 
Margaret Leinen, PhD.
Climate Response Fund
211 N. Union Street
Suite 100
Alexandria, VA 22314
P 202-415-6545
F 703-842-8031
mlei...@climateresponsefund.org



 From: Ken Caldeira kcalde...@carnegie.stanford.edu
 Reply-To: Ken Caldeira kcalde...@gmail.com
 Date: Thu, 18 Mar 2010 12:38:58 -0700
 To: geoengineering geoengineering@googlegroups.com
 Subject: [geo] Joe Romm post and comment on attending the Asilomar meeting
 
 http://climateprogress.org/2010/03/18/exclusive-chief-sponsor-of-landmark-clim
 ate-manipulation-conference-maintains-close-financial-ties-to-controversial-ge
 o-engineering-company/
 
 A part that quotes me:
 
 --
 
 *I have learned that the Asilomar geoengineering meeting is expected to play
 an important role in legitimizing and helping raise funds for Margaret
 Leinen's Climate Response Fund.*
 
 *I have not seen any statement from Margaret Leinen or her  Fund saying that
 the Fund will not support geoengineering field tests nor have I seen a
 statement saying that the Fund would not directly or indirectly transfer
 resources to for-profit companies like Climos.*
 
 *I am not comfortable with the the idea that a meeting set up to create
 guidelines governing geoengineering field tests might be used to help raise
 funds for geoengineering field tests, without the informed consent of
 meeting participants. I am also concerned with possible conflicts of
 interest related to the profit motive.*
 
 *Guidelines governing such tests should be developed as a product of an
 ongoing process involving established professional societies and
 organizations, established major non-profit institutions, intergovernmental
 institutions, or others who do not have an apparent stake in specific
 outcomes.*
 
 *Margaret Leinen can obviate my concerns by stating clearly  (1) that the
 Fund will not support geoengineering field tests and (2)  that the Fund
 would not directly or indirectly transfer resources to for-profit
 geoengineering companies like Climos (or other for-profit companies with
 significant financial participation by members of Margaret Leinen's family).
 *
 
 *Without such statements, I cannot be confident that I am not being used
 without my consent for purposes of which I do not approve. Thus, I cannot
 attend the meeting.*
 ---
 
 I would like to point out that the Scientific Organizing Committee for the
 Asilomar meeting is a stellar collection of people whose integrity is beyond
 reproach. I have no issue with the Scientific Organizing Committee. I simply
 fear that they too are being used to advance the goals of Margaret Leinen
 and her Fund.
 
 I have no fundamental problem with what is expected to occur within the
 meeting proper. My problem lies with the apparent attempt of Margaret Leinen
 and her Fund to use the credibility of the attendees and organizers of this
 meeting to legitimize her Climate Response Fund and help raise money for
 poorly defined purposes.
 
 ---
 
 Best,
 
 Ken
 
 ___
 Ken Caldeira
 
 Carnegie Institution Dept of Global Ecology
 260 Panama Street, Stanford, CA 94305 USA
 
 kcalde...@carnegie.stanford.edu
 http://dge.stanford.edu/DGE/CIWDGE/labs/caldeiralab
 +1 650 704 7212; fax: +1 650 462 5968
 
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RE: [geo] Geoengineering society - draft letter

2009-12-14 Thread David Keith
Institutions of this kind of work well when there are a large group of
experts who share roughly similar expertise and when the group acts
primarily as a value-neutral way to advance the discipline.

 

We are not remotely close to that stage for geoengineering.

 

If created now such a group would be primarily a lobby group, since
there are widely divergent views about what should be done on this topic
I see no chance that the group would be effective in speaking for a
broad community.

 

-David

 

 



From: geoengineering@googlegroups.com
[mailto:geoengineer...@googlegroups.com] On Behalf Of Ken Caldeira
Sent: December 13, 2009 5:32 PM
To: andrew.lock...@gmail.com
Cc: geoengineering
Subject: Re: [geo] Geoengineering society - draft letter

 

I am generally in favor of a bit of anarchy in science and technology,
and see institutions often as mechanisms that stifle creativity and
innovation.

What is the purpose of such an institution? What need is it trying to
fill?

How do you prevent the primary goal of the institution becoming its own
persistence and growth, regardless of how that might impact the stated
goals of the institution?

How do you prevent an institution from picking a few early winners and
then excluding ideas that come along later (that challenge statements of
institutional leaders, initial funding priorities, and assembled
constituencies)?

I am fine with people banding together to advance their specific goals.
I am skeptical about the need for an institution that attempts to speak
for everybody.



On Sun, Dec 13, 2009 at 10:49 PM, Andrew Lockley
andrew.lock...@gmail.com wrote:

I note the UK's IMechE http://www.imeche.org/ is currently a strong
supporter of geoengineering
http://www.imeche.org/about/keythemes/environment/Climate+Change/Geoeng

 

We have on several occasions suggested the creation of a 'geoengineering
institute' on this list.  I write today with an alternative suggestion.

 

My proposal is that we present a letter to the IMechE, signed by
prominent members of this list (especially those in the UK).  In this,
we would set out our plans for the institution, and ask that the IMechE,
with its existing infrastructure and recognition, will operate this new
geoengineering institution until such time as it is able to be 'spun
off' as an organisation in its own right.

 

My suggestion is that the letter should address the following points:

1) Setting out the principle of the organisation's existence as
a part of the IMechE

2) The creation of a specific class of memberships for
accredited and non-accredited geoengineers.

3) Defining the IMechE as the focal point for the study of the
regulation and systematisation of geoengineering.

4) Encouraging the model to be adopted internationally,
providing professional 'residence' to the geoengineering community
worldwide.

 

In my opinion, such a move is vital.  For too long, this community has
lacked a proper system of organisation, and I suggest that, after
several non-starter attempts to get things moving, we now look to an
established and sympathetic body to help systematise the discipline.

 

I look forward to receiving comments of all colours by return.

 

Thanks

 

A

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RE: [geo] Air Capture (re-naming the thread)

2009-12-11 Thread David Keith
Agreed. It's a hybrid. The thermo looks good, but kinetic and
mass-transfer limitations are severe. 

 

-D

 

 



From: geoengineering@googlegroups.com
[mailto:geoengineer...@googlegroups.com] On Behalf Of Ken Caldeira
Sent: December 11, 2009 2:16 AM
To: David Keith
Cc: Greg Rau; geoengineering@googlegroups.com
Subject: Re: [geo] Air Capture (re-naming the thread)

 

It's hard to see how the energy cost of the ocean alkalinity scheme can
get much below the cost of CaCO3 calcination .

What about using power plant flue gases to dissolve carbonates? That
seems to be an ocean alkalinity scheme that has energy costs well below
calcination.



___
Ken Caldeira

Carnegie Institution Dept of Global Ecology
260 Panama Street, Stanford, CA 94305 USA

kcalde...@carnegie.stanford.edu
http://dge.stanford.edu/DGE/CIWDGE/labs/caldeiralab
+1 650 704 7212; fax: +1 650 462 5968  





On Fri, Dec 11, 2009 at 11:33 AM, David Keith ke...@ucalgary.ca wrote:

Greg,

 

To me it's just the common definition; I did not intend to say anything
about relative merits. The topic was air capture and that seem enough
for one article. I think the geochemical approaches that involve adding
alkalinity to the oceans are worth serious work that's why I wrote the
article geochemical carbon management article. I have also pushed this
idea onto agendas at various research planning meetings (e.g., the NAS
advanced sequestration meeting), and we have considered adapting
calcination technology we develop for air capture to the CaO or MgO
scheme though we are not putting serious work into it. 

 

In my view there is no way to make a simple choice between them. There
are significant technical and institutional and governance challenges
with adding alkalinity to the ocean. On the other hand, restoring PH
could be a direct local environmental benefit. 

 

It's hard to see how the energy cost of the ocean alkalinity scheme can
get much below the cost of CaCO3 calcination and the electrochemical
schemes are expensive. One might argue, then, that air capture has lower
theoretical energy cost (10's of kJ/mol vs 100's) but no one knows how
to make the low energy AC work at low cost.

 

Bottom line: real development work is needed on both; they should be
linked where appropriate; and finally, it's far too early to pick
winners.

 

I know about the APS work, but I will reserve comments until it's out.
The real test will be in a few years when serious end-to-end engineering
cost estimates are made public. 

 

Yours,

D

 

 

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[geo] Air Capture

2009-12-10 Thread David Keith
Short answer: no, not with business-as-usual rules for permitting and
siting. Even with money, it's all but impossible to develop deployable
industrial hardware of the kind we are talking about here in five years.


 

Alternative-world answer: Under wartime style system in which multiple
independent technological pathways were pursued at once and if local
planning and environmental permitting rules were suspended, then yes.

 

Question: why would it ever make any sense to do this? The carbon cycle
inertia is large. It is cheaper to get started by just cutting emissions
using tools we already have from efficiency to carbon free electricity
by wind, nuclear or coal-with-capture. Air capture is useful only after
some of the easy stuff has already been done. 

 

-D 

 



From: Manu Sharma [mailto:orangeh...@gmail.com] 
Sent: December 10, 2009 7:54 AM
To: David Keith
Cc: Geoengineering
Subject: Re: [geo] Prof. Klaus Lackner + air capture demo at AGU in SF

 

Having read your overview in Science now, please disregard my second
question about cost. 

 

I'd re-frame the first question as: 

 

If government funding is made available to the existing labs and
new research institutions around the world, with the aim to make a
concerted effort focussed on large-scale deployment, is it foreseeable
to imagine air capture ready to be deployed within five years? 

 

Thanks,

Manu

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[geo] Recent meetings

2009-12-07 Thread David Keith
Here are notes on a three recent meetings

 

1.  Video's and slides of the October 30th MIT symposium are here:

eathttp://web.mit.edu/esi/symposia/symposium-2009/symposium2009-presenta
tions.html

 

2.  There was a two day meeting at Max Planck Hamburg 25 and 26th
November. See attached agenda. This meeting launched a major (~ 1m euro)
multi-institution initiative on geoengineering that will focus primarily
on climate modeling of SRM techniques. Among other things progress was
made on the specification of standard experiments examining GCM
responses to stratospheric aerosol geoengineering proposed as a CMIP-5
project by Alan Robock.  

 

3.  Finally, the on 27th November the University of Heidelberg
kicked off an interdisciplinary initiative on The Global Governance of
Climate Engineering. This well funded (~ 1m euro) project involves the
Max Planck Institute for International Law, along with researchers from
many disciplines including economics, atmospheric physicists, and human
geography. There is a very brief German description following the link
on the upper right of this page: 
http://www.marsilius-kolleg.uni-heidelberg.de/index_en.html
http://www.marsilius-kolleg.uni-heidelberg.de/index_en.html 

 

 

 

 

 

 

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Agenda-Geoengineering-HSt-181109.pdf
Description: Agenda-Geoengineering-HSt-181109.pdf


RE: [geo] What if Earth had rings like Saturn?

2009-11-23 Thread David Keith
Even where this not a joke, there is a problem. When I first got
interested in this topic about 1990 one of the first things I did was
look at the NAS estimates about orbiting mirrors or scatters. Problem is
if you use mass-efficient scatterers they are rapidly blown out of orbit
by light pressure.

 

The Russin and Flit book worth a look. There are earlier soviet
reference as well. It was the engineered everything era.

 

-David

 

 



From: kcalde...@gmail.com [mailto:kcalde...@gmail.com] On Behalf Of Ken
Caldeira
Sent: November 23, 2009 3:21 PM
To: dan.wha...@gmail.com
Cc: geoengineering
Subject: Re: [geo] What if Earth had rings like Saturn?

 

When I was a post-doc at Penn State working with Jim Kasting we did
calculations of changes in solar flux from rings as a possible
explanation of low-latitude glaciations in the ancient past, but we
didn't published them. I think we decided you would need quite a ring to
freeze the equator. At that time we were not interested in more subtle
effects.

Here is a manuscript that looks at the issue. I haven't looked at it
carefully to see if it is right:
http://www.star-tech-inc.com/papers/earth_rings/earth_rings.pdf

Of course, an equatorial ring would shade only the winter hemisphere.

___
Ken Caldeira

Carnegie Institution Dept of Global Ecology
260 Panama Street, Stanford, CA 94305 USA

kcalde...@ciw.edu; kcalde...@stanford.edu
http://dge.stanford.edu/DGE/CIWDGE/labs/caldeiralab
+1 650 704 7212; fax: +1 650 462 5968  




On Mon, Nov 23, 2009 at 1:41 PM, Dan Whaley dan.wha...@gmail.com
wrote:

Just for laughs...

This is wonderful eye candy.

http://idealog.co.nz/blog/idealist/rings-around-planet-earth

Of course the question is how much cooling would they provide.   It
would be permanent of course.  (Ah well...)

Great to see the 3D renderings from the POV of different cities and
different times of day

Enjoy.

Dan

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RE: [geo] Re: Rejected - a simple argument for SRM geoengineering

2009-11-20 Thread David Keith
Greg

 

GWP's by design ignore all climate impacts beyond 100 years. 

 

This has real consequences as it makes methane look relatively more
important that it should be, and it also overweight's the beneficial
impacts of biomass sequestration in some calculations.

 

While some traditional economists may assume that discounting allows
them to ignore any impact beyond 100 years, this GWP formula has long
been a point of contention as most of us do value the future of the
planet beyond 100 years.

 

Adopting a 100 year analysis horizon, as the IPCC generally does, takes
our eye off the long term consequences of dumping fossil carbon in the
atmosphere. The risk of sea level rise look much less serious if one
only looks a century out. 

 

Scientific understanding about the long term impacts of fossil emissions
is decades old (see Jim Kasting's old papers for example), popular
realization of these facts is long overdue. 

 

Cheers,

David

 

 



From: Greg Rau [mailto:r...@llnl.gov] 
Sent: November 16, 2009 1:23 PM
To: mmacc...@comcast.net; geoengineering@googlegroups.com
Subject: Re: [geo] Re: Rejected - a simple argument for SRM
geoengineering

 

In light of recent modeling results on the lifetime of CO2 in the
atmosphere, I am concerned that the current time-integrated (not
instantaneous) GWP estimate for CO2 has been underestimated and hence
GWP's of other gases (esp short-lived gases) relative to CO2 have been
overestimated.  E.g., Eby et al., 2009:

http://ams.allenpress.com/perlserv/?request=get-abstractdoi=10.1175%2F2
008JCLI2554.1

show that 20-30% of excess emissions of CO2 and 60-70% of the subsequent
CO2-caused surface air temp anomally exists 10,000 years after emission.
Isn't this (or is this?) a far larger total time-integrated GW effect
than a mass equivalent emission of CH4?  Experts please set me straight.

Thanks,

Greg  

 

Agreed, one has to consider a time period, so assume one takes a
day that when injected there is no decay over this period-so it might as
well be a second of time one takes-so virtually instantaneous. And I'll
assume linearity on methane absorption and logarithmic for CO2.

So, for methane, humans have caused an increase of roughly 1000
ppb which converts to about 3 GtCH4, and this causes a forcing of about
0.5 W/m**2 (at the tropopause) per IPCC.

For CO2, we know that a doubling (so we'll say from 300 to 600
ppm so we are in the range of interest) causes a forcing of about 3.6
W/m**2 (at the tropopause). So, 300 ppm of CO2 in the atmosphere is
roughly 600 GtC or 2200 GtCO2 (and global warming potential is done for
CO2, I believe.

So, if we take the ratio of forcing to mass for CH4 divided by
the ratio of forcing to mass for CO2, we get a rough estimate of the
instantaneous GWP, so

[0.5/3]/[3.6/2200] equals roughly 100

for the ratio at t=0 (so allowing for no decay) of the radiative
forcing caused by a unit mass of CH4 added to the atmosphere to a unit
mass of CO2 added to the atmosphere.

Not exact, but plausible.

Mike




On 11/16/09 3:42 AM, Peter Read pre...@attglobal.net wrote:

John, Andrew
Re BTW, does anybody know the _immediate_ warming potential of
methane?
Someone will correct me no doubt but my understanding is that
warming is a rate process measured in W/m^2
So instantaneous [[== immediate?]] warming is an incorrect
concept
Unless it continues for a second, a week, a year, 25 years, for
whatever, no warming takes place.
So it is necessary to multiply by a duration to get joules/m^2
It's how many joules get into the low albedo meltwater on top of
Greenland's ice that decides how much gets melted each year to fall down
crevasses and lubricate the eventual collapse of large areas of ice into
the oceans.  
Meaning that the integral [[roughly]] under the CO2 level curve
is what matters [multiplied by the warming potential over that period]
when it comes to measuring threats of Greenland's collapse
So the key issue is duration - how long elevated greenhouse gas
levels last and how to get them down.
Think that's right
Peter


- Original Message -
 
From:  John Nissen mailto:j...@cloudworld.co.uk
mailto:j...@cloudworld.co.uk
 
To: andrew.lock...@gmail.com
 

Cc: geoengineering
mailto:geoengineering@googlegroups.com
mailto:geoengineering@googlegroups.com   
 
Sent: Monday, November 16, 2009 6:18  PM
 
Subject: Re: [geo] Re: Rejected - a  simple argument for
SRM geoengineering
 


Hi Andrew,

You say:  I don't oppose John's argument, but 

[geo] Re: Sea ice: beware of hype, uncertainty cut's both ways

2009-11-03 Thread David Keith
John

 

We are generally in good agreement.

 

The one point where we disagree is about how climate sensitivity is
introduced into models. There is no knob for climate sensitivity in a
GCM. There are many processes which are strongly nonlinear from the
initiation of convection to parameterizations of sea ice and snow
reflectivity. Climate sensitivity is the way we talk about (and measure)
the overall response of the model to perturbations such as changes in
CO2 or insolation. This is not a claim that models get it all right or
that they have the sensitivity right. But it's wrong to say that models
don't have the nonlinearities you described. They do, and they have for
decades. It may be that they don't have them in the right way or the
overall sensitivity is too high, on the other hand it may be the over
all sensitivity is too low.

 

While it's clear that there are many relatively sharp tipping points
when it comes to particular climate impacts (e.g., the temperature and
precipitation regime at which a particular species of tree does or does
not thrive, or the conditions that make and I sheet grow or shrink), but
there is substantial evidence that the climate system as a whole both in
reality and in models response relatively linearly to perturbations and
that it may be that very strong nonlinearities tipping points are not
particularly important in understanding the risks of climate change at
large-scale. Obviously this is a point on which people have different
views, but there many people in the core the climate modeling community
who would share the view I just gave despite the hype about tipping
points.

 

The most important tipping point seems to involve the North Atlantic
overturning circulation, and that may have had something to do with
mediating the instabilities between glacial interglacial states, however
it is less reason to believe that this instability will operate between
the current climate and warmer climates. We had this conversation the
MIT meeting and Dave Battisti expressed exactly this view.

 

This is not in any way to minimize climate risks, the simple fact of
very large uncertainty in the overall climate sensitivity combined with
the uncertainties in nonlinearities in many of the impacts means that
there is a significant chance of dramatic even for some of us
catastrophic climate impacts with the current CO2 trajectory. It's
just a statement that you don't need to overdo the idea of tipping
points to see this.

 

 

 

Yours,

David

 



From: geoengineering@googlegroups.com
[mailto:geoengineer...@googlegroups.com] On Behalf Of John Nissen
Sent: November 2, 2009 4:10 PM
To: David Keith
Cc: climateintervent...@googlegroups.com;
geoengineering@googlegroups.com; Ken Caldeira; Julian Norman; Mike
MacCracken
Subject: [geo] Re: Sea ice: beware of hype, uncertainty cut's both ways

 


Thank you, David, for your thoughtful reply and the excellent points you
make, which culminate in an acknowledgement of the argument for albedo
geoengineering to save the Arctic sea ice, as I have been proposing.
Your support is most welcome.

Re your point 1, the proposal does not assume a particular estimate for
date of disappearance of Arctic sea ice.   There are two arguments here.
The first is that it better to apply the geoengineering before the
positive feedback grows any stronger.  (As Mike puts it, it is better to
put out a small fire rather than wait until the whole building is
aflame.)  The second argument is to take the precautionary principle,
and consider the soonest time for disappearance within the possible
range of times.  Here the very uncertainty that you highlight is giving
us a significant probability of ice summer disappearance within a few
years, even if the most likely date (aka median date) may be a few
decades away. 

Re point 2 and the models, the typical models give a climate
sensitivity factor, which is essentially linear and assumes tipping
points are not reached.  However, with the Arctic sea ice we may be
seeing tipping already in progress, due to non-linear effects and
positive feedbacks which are notoriously difficult to model.
Furthermore, the Arctic sea ice may never have totally disappeared in
any interglacial period of the past 2 million years; and the maximum
temperature of recent interglacial periods will soon be exceeded.   So
we are moving into uncharted waters.  Thus the assumption that global
warming will proceed linearly with CO2 (i.e. with constant climate
sensitivity factor) seems debatable.  Therefore there is all the more
reason to try and save the Arctic sea ice.

Re point 2 and the methane, again one could argue for a precautionary
approach.  Some scientist estimate that there is enough methane to more
than double GHG forcing if it were released.  Halting the Arctic warming
would greatly reduce the risk.

Re point 3, it is good to see that experts from IPCC now acknowledge
that they grossly underestimated the risk

[geo] Re: Arguments against geoengineering

2009-11-02 Thread David Keith

I think the idea that fossil resources will provide a meaningful constraint on 
CO2 emissions does not pass a fact checker's laugh test. We have enough carbon 
within the growing reach or our extraction technologies to push CO2 
concentrations beyond 5,000 towards 10,000 ppm.

For my own lay-language debunking of this idea in a popular book see:

Keith, David. (2009) Dangerous Abundance. IN: Homer-Dixon, T.  Garrison, N. 
(Eds.) Carbon Shift: How The Twin Crises Of Oil Depletion And Climate Change 
Will Define The Future, Toronto: Random House of Canada, pp26-57.

Available at: http://people.ucalgary.ca/~keith/Preprints.html. 

-David

-Original Message-
From: geoengineering@googlegroups.com [mailto:geoengineer...@googlegroups.com] 
On Behalf Of Christopher Mims
Sent: October 30, 2009 7:35 AM
To: geoengineering
Subject: [geo] Re: Arguments against geoengineering


Emissions in 2020  emissions in 2010 also assumes that there is
nothing that would limit the material inputs that will lead to those
emissions. You don't have to be a disciple of 'limits to growth' to
recognize that at some point, we'll start bumping our head against a
ceiling determined by the carrying capacity of the planet.

Even the conservative IEA believes that maximum historical production
of liquid fuels (peak oil) will arrive within the next decade.

If you believe more pessimistic estimates, net production of liquid
fuels has already peaked (2008) and our civilization's near total
dependence on oil for transportation means emissions from the
transportation sector will only shrink going forward.

Whether or not any of this is true is anyone's guess - but it is an
example of an X factor, beyond technology, that is within the realm of
possibility.

(Another, and related, X factor is a second or an ongoing global
recession. Just look at what the one we're in now did to global CO2
emissions.)

In other words, legislation and conservation is not the only thing
that will determine maximum annual CO2 emissions from anthropogenic
sources - in fact these might be the two factors that are *least*
likely to determine the ultimate level of those emissions.

On Oct 30, 8:42 am, Alan Robock rob...@envsci.rutgers.edu wrote:
 Dear Dan,

 Dangerous anthropogenic inteference is now commonly defined as 2°C
 about preindustrial global average temperatures (about 1°C above current
 levels).  Certainly it is not a step function, and impacts increase with
 temperature change, and we are already experiencing some.  So we need a
 lot of adaptation, too.

 Alan

 Alan Robock, Professor II
    Director, Meteorology Undergraduate Program
    Associate Director, Center for Environmental Prediction
 Department of Environmental Sciences        Phone: +1-732-932-9800 x6222
 Rutgers University                                  Fax: +1-732-932-8644
 14 College Farm Road                   E-mail: rob...@envsci.rutgers.edu
 New Brunswick, NJ 08901-8551  USA      http://envsci.rutgers.edu/~robock



 On Fri, 30 Oct 2009, Dan Whaley wrote:

  Alan,

  I agree that 450 or 500 are theoretically achievable with emissions
  reductions-- clearly.  (Though either would effectively require
  immediate and aggressive reductions from everyone, now).

  But if we're already seeing impacts we don't like, and we know the
  impacts considerably lag the forcing, what leads us to believe these
  are acceptable levels?

  Dan

  On Oct 29, 7:18 pm, Alan Robock rob...@envsci.rutgers.edu wrote:
  Dan,

  Where do you think we need to be?  And when?  If it is 350 ppm soon, of
  course not.  That would take massive carbon capture from the atmosphere
  and very rapid reductions in emissions.  But if you want to stop
  somewhere between 450 and 500 ppm, adapt, and then gradually reduce the
  concentration with carbon capture, I think we can do that with carbon
  capture from the stacks of coal-fired plants, and rapid transition to an
  electric economy with solar and wind generation.  It would need a
  substantial and regular increase in the price of carbon emissions.  Not
  being a political scientist, I cannot predict how likely this is, not
  that political scientists can either, but it is certainly possible.

  If climate change is the greatest threat to world security, the
  resources now being spent on the military (and half of the scientists
  and the engineers in the US working for them) can certainly be
  redirected to this goal.  We need not accept the status quo as a
  predictor of the future.

  Alan

  Alan Robock, Professor II
     Director, Meteorology Undergraduate Program
     Associate Director, Center for Environmental Prediction
  Department of Environmental Sciences        Phone: +1-732-932-9800 x6222
  Rutgers University                                  Fax: +1-732-932-8644
  14 College Farm Road                   E-mail: rob...@envsci.rutgers.edu
  New Brunswick, NJ 08901-8551  USA      http://envsci.rutgers.edu/~robock

  On Thu, 29 Oct 2009, Dan Whaley wrote:

  

[geo] Re: Royal Society report - Temperature rebound a myth?

2009-09-07 Thread David Keith

My two bits into this interesting debate:

On the temperature rebound. As Ken says, there is no question that the
temperature rebound is real. Simple physics tells you it should be
there, and this is confirmed by experiments with at least three
different GCMs.

The question is: is it a bug or a feature? I lean towards feature, and
I don't take the termination risk all that seriously. 

One of the central advantages of SRM geo is the speed of action. In
simple economic formulations it is the speed that is the principal value
because you can decide how much to implement after uncertainty about
climate sensitivity is resolved (See #117 at
www.ucalgary.ca/~keith/geo.html). You could also shut it off if
something goes wrong. Yes, I know about hysteresis but having fast
control is still better than not having it.

In a recent debate about this topic someone proposed three example
scenarios were one would consider fast response a termination risk: 

Possible reasons for early and rapid termination would include (e.g.)
ocean acidification proves to be much worse than expected, deleterious
health or ecological effects of less direct radiation are discovered
(think about bees), ditto for high CO2 on plants or insects, the future
world government is taken over by religious maniacs who consider SRM to
be a violation of Gaia, or something like that, etc etc.

I still don't see it as a risk. Here are my three answers from that
debate:

1. If we find that the effects of high CO2 on ocean plants or insects
are intolerable, then we need a crash program on negative emissions:
biomass with capture, burying trees, putting alkalinity in the oceans.
Halting SRM will not help; indeed it may hurt since there is evidence
that some SRM may slightly increase NPP so slightly increasing carbon
flux to biosphere. 

This is the most common and seemingly credible concern regarding
termination risk but, in my view, it confuses cause with effect. Even
if it's true that one has decided to put more CO2 in the air because of
SRM (that is, SRM as cause) the discovery that the CO2 is more dangerous
than expected (the effect) is a reason to focus on CDR not to stop SRM.

2. If religious maniacs take over the government I think the problem is
religious maniacs not the reversibility of SRM. This scenario boils down
to saying that the danger is that we will decide to turn it off. But in
my mind is that doesn't count a risk. 


I like having an adjustable thermostat my house. Of course, there's some
chance that my 12-year-old will decide to turn it all the way down in
protest against the evils of parental rule. However, on can see this as
a risk associated with the thermostat or a risk of having rowdy kids. If
this is a risk it's the precise converse of a benefit.

3. Given that there are many methods to achieve SRM, and given that as
we described in the Novim report, one would gradually work our way up to
full scale, I find it hard to imagine a scenario in which it was
suddenly reveal that there was a danger with a particular method that
did not allow substitution of a alternate method. 

Suppose the engineered nanoparticles deadly cancer after a 10 year
incubation period? Under the slowly work your way up scenario while the
discovered the deaths a decade before you went to full-scale. But
ignoring that; and assuming one suddenly figures out that the engineered
particles must be taken out one could go back to just plain sulfur. We
know that sulfur doesn't have a similarly obscure deadly effect since we
tried it with Pinatubo.


That said, it is of course true that the possibility of rapidly
modulating the climate poses risks in a world with many competing
actors. 

If the drivers are fighting, ut's more dangerous to be in a
high-performance sports car then in an old clunker with stiff steering
response. 

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[geo] Re: Royal Society report - Temperature rebound a myth?

2009-09-07 Thread David Keith

Greg,

Let me push back a bit. I absolutely agree that experiments are crucial and 
that by working our way up in experimental scale we will learn more and 
therefore reduce risk. While we did not say this as clearly in the RS report as 
we might have, and not as clearly as in Novim, I don't believe the RS 
contradicts this view.

Also, I and several others of the report have more experience as 
experimentalists than as modelers.

Cheers,
D



-Original Message-
From: geoengineering@googlegroups.com [mailto:geoengineer...@googlegroups.com] 
On Behalf Of xbenf...@aol.com
Sent: September 6, 2009 12:30 PM
To: j...@cloudworld.co.uk; kcalde...@stanford.edu
Cc: geoengineering@googlegroups.com; wig...@ucar.edu; s.sal...@ed.ac.uk
Subject: [geo] Re: Royal Society report - Temperature rebound a myth?



Throughout these studies, few realize that this is engineering. 
Learning how the global system operates is best accomplished by 
experiments that scale up as we learn, accompanied by simulations. 
Issues of risk are nearly meaningless at early stages. Real risk falls 
as you learn.

The death rate in aviation in its first decade was nearly 10%! Still, 
people did it.

Nor does the RAS report seem to understand how scaling of experiments 
works. Maybe that's because few of them have ever done lab experiments; 
simulations are a very different game--a form of theory, really.

Gregory Benford


-Original Message-
From: John Nissen j...@cloudworld.co.uk
To: Ken Caldeira kcalde...@stanford.edu
Cc: Geoengineering geoengineering@googlegroups.com; Tom Wigley 
wig...@ucar.edu; Stephen Salter s.sal...@ed.ac.uk
Sent: Sun, Sep 6, 2009 11:12 am
Subject: [geo] Re: Royal Society report - Temperature rebound a myth?






Hi Ken,



We may disagree about the rebound of SRM termination, but we agree
about the sense.  Indeed turning off SRM has been likened to turning
off the kidney dialysis machine of a patient with kidney failure. 
(Thanks, Stephen, for that thought.)



So why did the Royal Society report mark Stratospheric aerosols with
an H for high risk in table 3.6; and 2/5 for safety in table 5.1?  You
were a member of the working group!



I note that Cloud albedo al
so gets an H for Regional climate
change.  But isn't that a huge advantage of the method over
stratospheric aerosols - that it can be more targeted to cool
particular areas?  Every way that a method can be tuned, or targeted
more closely, means that there is more scope for avoiding side-effects
- thus is a safety bonus.  (Being able to turn off the SRM may also
allow you to react to unexpected side-effects - another bonus.)



Cheers,



John



---



Ken Caldeira wrote:
See attached paper ...



If you turn off solar deflection you would get rapid warming (no
overshoot, but a rapid rebound).



This is not a myth that needs refuting.



The question is:  What does this mean?



There are plenty of things that we do that, were they stopped suddenly,
we would be in big trouble.



For example, if we stopped pumping oil today, our transportation system
and therefore food distribution system would grind to a halt and there
would be mass starvation. Does this mean that it would be crazy to base
a food distribution system on oil? Or does it mean, if you are going to
base a food distribution system on oil, you had better be pretty sure
you can assure a nearly continuous flow.



I think the rapid rebound means that everyone will be incented to make
sure that the amount of solar radiation deflection is modulated with=0
D
care. The fact that stopping SRM suddenly could bring big problems
means that we would take great care not to stop suddenly.



If we stopped generating electricity we would be in big trouble. If we
stopped piping water we would be in big trouble. If we stopped hauling
garbage we would be in big trouble. Etc, etc.



Our response to these threats is not to say: no electricity, no water
pipes, no garbage hauling, etc. Instead we say, let's assure
continuity, as best we can, of electricity, water piping, garbage
hauling, etc.




___

Ken Caldeira



Carnegie Institution Dept of Global Ecology

260 Panama Street, Stanford, CA 94305 USA



  kcalde...@ciw.edu;
  kcalde...@stanford.edu

  http://dge.stanford.edu/DGE/CIWDGE/labs/caldeiralab

+1 650 704 7212; fax: +1 650 462 5968  







   On Sun, Sep 6, 2009 at 8:38 AM, John Nissen 
lt;j...@cloudworld.co.ukgt;
wrote:




At the launch of the Royal Society report, it was explained that a
disadvantage of SRM was if you suddenly stopped it, because the
temperature would rebound due to all the CO2 that had accrued in the
meantime, with its suppressed warming effect.  This termination
effect is expressed as a high risk, see table 3.6 [1]  with footnote
[2].



It so happens I have just looked through Tom Wigley's file on the
geoengi
neering googlegroup:

http://groups.google.com/group/geoengineering/files




In this presentation he 

[geo] Research Councils UK Energy Programme announces funding support for Geoengineering research

2009-09-04 Thread David Keith
http://www.rcuk.ac.uk/news/090901.htm


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[geo] Re: Fwd: costs of air capture - Royal Society report

2009-09-03 Thread David Keith
Roger,

 

It was a group report, while I contributed to the air capture section we
were careful that I did not have final word since I have a strong
self-interest in making air capture look good.

 

I certainly know about your work and it came up in discussions about air
capture in the group.

 

I don't think your paper contradicts the RS summary, but I suggest we
take that conversation off-line to get some resolution.

 

I don't think there is a simple cost-benefit analysis argument that
distinguishes between carbon reduction and solar radiation management,
they are apples and oranges. Reducing emissions and /or carbon removal
is a necessary but not sufficient response to climate risk, but given
the uncertainty in the climate's response to CO2 and we cannot be sure
that emission reductions alone will allow us to avoid dangerous climate
risks. This is true even when one includes carbon removal because of the
technological and carbon cycle inertia. SRM is fast and cheap, yet it
cannot fully compensate for the climate risk of elevated carbon dioxide.
SRM is sufficiently cheap that decisions about its use will almost
certainly be risk-risk decisions not cost-benefit decisions. 

 

See, for example, the geo decision analysis preprint, #117 on the geo
section of my site: www.ucalgary.ca/~keith/geo.html 

 

On air capture, I have a perspective that will be out in two weeks in
Science. 

 

Yours,

David

 

 



From: geoengineering@googlegroups.com
[mailto:geoengineer...@googlegroups.com] On Behalf Of Ken Caldeira
Sent: September 3, 2009 7:58 AM
To: geoengineering
Subject: [geo] Fwd: costs of air capture - Royal Society report

 

on behalf of Roger Pielke Jr

[ In brief reply: With David Keith as co-author of the report, we relied
heavily on his assessment in this area. -KC]


All-

It is interesting that my paper on the costs of air capture was
ignored by the Royal Society committee on geoengineering (as I am told
by a member that it was made available to the Committee, and it is the
only such effort focused on comparing costs to IPCC and Stern-type
estimates):

Pielke, Jr., R. A., 2009. An Idealized Assessment of the
Economics of Air Capture of Carbon Dioxide in Mitigation Policy
http://sciencepolicy.colorado.edu/admin/publication_files/resource-2716
-2009.03.pdf , Environmental Science  Policy, Vol. 12, Issue 3, pp.
216-225.

Perhaps the Committee thought the analysis was so deeply flawed
as to not be of value (??  If so, none has yet shared this perspective
with me).  Even so, surely the readers of the report would have
benefited from hearing in what ways the paper is flawed rather than just
pretending that it does not exist.  Instead of the RS providing a
comprehensive review, there exists a peer-reviewed paper on the costs of
air capture that contradicts some of the views on air cpature costs
expressed in the RS report (maybe that is the explanation).  To the
outsider it does make the Committee look uniformed or
less-than-comprehensive. 

Perhaps the members of the committee on this list might want to
comment?

I offer some comments here:


http://rogerpielkejr.blogspot.com/2009/09/air-capture-in-royal-society.h
tml

In other news, yesterday I argued in terms of cost-benefit
analyses against SRM and in favor of AC as a tool in the climate policy
tool box before Bjorn Lomborg's panel of Nobel Prize winning economists.
They are supposed to report out tomorrow, and we'll see what they come
up with.  Lomborg has been writing op-eds suggesting that SRM could be
an alternative to conventional mitigation.  I strenuously opposed this
view before the panel.

I'll comment about the process on my blog from my vantage point
upon release of the report.

Best regards,

Roger

Roger Pielke, Jr.
University of Colorado

 





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[geo] Re: ETC Group on Royal Society Report: The Emperor's New Climate: Geoengineering as 21st century fairytale

2009-08-31 Thread David Keith

Diana,

Call me old-fashioned, but I believe deeply in the virtues of
transparency and honesty in debating matters as important as this. I
welcome skepticism about geoengineering. 

However, the disconnect between your press release and what is actually
being suggested by the Royal Society report, or for that matter your
private comments to me at the NAS meeting are disappointing. The way the
ETC group has managed this, suggest to me not skepticism but its precise
opposite closemindedness. I suspect that you don't want to live in a
world where debate gets reduced to soundbites and interest group fight
to distort facts to the maximum yet seems to me that is where the ETC
Group is leading here. Why for example release a commentary with ad
hominem comments like tricksters before you have even had a chance to
look at the Royal society report. 

I note that ETC has a base in Ottawa, my hometown, and you could easily
have taken the time to talk to me (as I have offered), but instead it
seems that ETC would prefer to hold strong opinions without actually
engaging substantively with other views.

Is this really how you want to see public debate on important issues?

Yours,
David


-Original Message-
From: geoengineering@googlegroups.com
[mailto:geoengineer...@googlegroups.com] On Behalf Of Diana Bronson
Sent: August 28, 2009 1:35 PM
To: geoengineering@googlegroups.com;
climateintervent...@googlegroups.com
Subject: [geo] ETC Group on Royal Society Report: The Emperor's New
Climate: Geoengineering as 21st century fairytale


ETC Group
News Release
28 August 2009
www.etcgroup.org


SCIENCE FICTIONS: UK'S ROYAL SOCIETY TO ISSUE MAJOR REPORT
ON GEOENGINEERING SEPTEMBER 1;
BAN REAL-WORLD EXPERIMENTS, SAYS ETC GROUP

The oldest scientific academy in the world, the UK's Royal Society,
will release its long-awaited report on geoengineering September 1st
2009 in London. The report, drafted by a panel dominated by
geoengineering enthusiasts, is widely expected to recommend that the
government support more research and perhaps even real-world
experimentation of these controversial new technologies that
intentionally manipulate the earth's climate on a large scale with the
aim of lessening the effects of climate change.

Geoengineering is a bad idea, and, unfortunately, it may transform
Lord Rees's book from musings to memoir, says Diana Bronson,
researcher for the international technology watchdog ETC Group,
referring to the Royal Society President's 2004 book, Our Final
Century, which suggested that humans may not live to see the end of
the 21st century.

Geoengineering can refer to sulphate-injections in the stratosphere
and cloud-whitening to reflect sunlight away from the earth,
fertilization of the oceans with iron nano-particles to try to
increase their carbon-carrying capacity, intentionally modifying
global weather patterns, among other techniques.

The Royal Society may be cautious in their report but, in fact, when
it comes to geoengineering, a yellow light can quickly turn green. For
the climate to take notice, any geoengineering scheme would have to be
massive - sulphate particles or whitened clouds would have to deflect
a lot of sunlight and ocean fertilization would have to cover great
swathes of sea. Even the most careful computer models won't be able to
predict what will happen if an experiment is scaled-up and moved out
of doors, argues Bronson. If governments believe there is a techno-
fix to the climate change conundrum that will let them off the hook at
the climate change treaty negotiations in Copenhagen, they will throw
precious time and dollars at sci-fi fantasies, overlook potentially
devastating side effects and divert their attention from the urgent
need to reduce carbon emissions at source.

ETC Group's new special report, The Emperor's New Climate:
Geoengineering as 21st century fairytale, questions the narratives
commonly used by the geoengineering lobby to advance their agenda.
Contrary to what geoengineers are saying, this is a costly time-
waster, says Bronson. The report calls for a broader international
discussion and concludes that any effort to experiment these
technologies in the real world is nothing short of geopiracy and
should be banned.

ETC Group's special report, The Emperor's New Climate: Geoengineering
as 21st century fairytale, is available on the Internet at
http://www.etcgroup.org/en/materials/publications.html?pub_id=762


-30-

For more information:

Diana Bronson (Montreal, Canada) di...@etcgroup.org
Phone: +1 514 273 6661; cell +1 514 629 9236

Kathy Jo Wetter (Durham, NC, USA) k...@etcgroup.org
Phone: +1 919 688 7302

Silvia Ribeiro (Mexico City) sil...@etcgroup.org
Phone: 011 52  6326 64

Molly Kane (Ottawa, Canada) mo...@etcgroup.org
Phone: +1 613 241 2267, ext 26; cell +1 613 797-6421




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[geo] Re: Ecologists weigh in

2009-08-23 Thread David Keith
-scale geoengineering scheme is fertilizing the oceans with
iron to increase carbon uptake from the atmosphere. Charles Miller of
Oregon State University says that ocean fertilization could create a
rise in iron-limited phytoplankton populations, which by dying and
sinking would use enough oxygen to create extensive dead zones in the
oceans. In addition, he says, the maximum possible rate of ocean iron
fertilization could only offset a small fraction of the current rate of
carbon burning by humans.

Ocean fertilization also does not alleviate the increasing problem of
ocean acidification, caused by carbon dioxide from the increasingly
carbon-rich atmosphere dissolving into seawater. In fact, Miller says,
ocean fertilization schemes will likely exacerbate this problem.

Any large-scale fertilization could cause risks to ocean ecosystems as
great as those of global warming itself, he says.
Despite its apparent hazards at the global scale, Jackson thinks that
research should continue on safer ways to use geoengineering at a
smaller scale. Geologic sequestration, sometimes known as CO2 capture
and storage, takes CO2 out of the atmosphere and stores it in
underground reservoirs. Jackson says that this solution has the
potential to store more than a century's worth of electric power
emissions at a relatively low cost. He notes, however, that some
potential risks of geologic sequestration include carbon leakage and the
potential for interactions with groundwater.
But on the planetary scale, most ecologists are skeptical of climate
engineering.

Playing with the Earth's climate is a dangerous game with unclear
rules, says Jackson. We need more direct ways to tackle global
warming, including energy efficiency, reduced consumption, and
investment in renewable energy sources.
###
Clifford Duke, Director of Science Programs at the Ecological Society of
America, is co-organizer of the symposium. Additional speakers include
David Keith from the University of Calgary and Phillip Duffy from
Climate Central, Inc.
The researchers will present their results in:
Symposium 21 - The Environmental Effects of Geoengineering
Thursday, August 6, 2009, 1:30 PM-5:00 PM
Pecos room, Albuquerque Convention Center
For more information about this session and other ESA Annual Meeting
activities, visit http://www.esa.org/albuquerque. The theme of the
meeting is Ecological Knowledge and a Global Sustainable Society. More
than 3,500 scientists are expected to attend.
The Ecological Society of America is the world's largest professional
organization of ecologists, representing 10,000 scientists in the United
States and around the globe. Since its founding in 1915, ESA has
promoted the responsible application of ecological principles to the
solution of environmental problems through ESA reports, journals,
research, and expert testimony to Congress. ESA publishes four journals
and convenes an annual scientific conference. Visit the ESA website at
http://www.esa.org.

Subscribe to ESA press releases by contacting Christine Buckley.





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[geo] Re: The International Maritime Organisation's plans to warm the world

2009-08-23 Thread David Keith
A few comments.

 

1.  Am CCing my colleague Jim Corbett, who wrote a bunch of the
important papers on emissions from shipping, is an author of the latest
paper mentioned her, and as worked with the IMO on this. Jim: any
discussion on this tradeoff at IMO?

 

2.  Some ships already dual fuel (bunkers and natural gas), where
the NG is burned in and near port to comply with local air quality.

 

3.  Numbers only work against bifurcated system if no policy to
preserve or promote sulfur emissions in open ocean. 

 

4.  Work needed to estimate the ratio of climate forcing to heath
impacts of S emissions as a function of the location of the emissions,
this would allow where it make most sense to promote or restrict
emissions. I will pitch this to atmo chemists at their Gordon Research
conference this evening. 

 

5.  We don't just want to leave ship emissions as they are because
we will need manage NOx even if we want S emissions. Both are big from
ships. See Jim's paper:  J. J. Corbett and  P. S. Fischbeck, Emissions
from Ships, Science, vol. 278, no. 31 October 1997, pp. 823-824. 

 

6.  The idea that we can use the S for geo is likely irrelevant.
There is ample S as H2S in sour gas either produced and re-injected or
made into elemental S using Claus process. (There are many megaton-scale
blocks of elemental S from this process in Alberta where I live,
stunning yellow patches on the landscape.)

 

-David



From: geoengineering@googlegroups.com
[mailto:geoengineer...@googlegroups.com] On Behalf Of Alvia Gaskill
Sent: August 20, 2009 1:07 PM
To: kcalde...@stanford.edu; geoengineering; Climate Intervention
Subject: [geo] Re: The International Maritime Organisation's plans to
warm the world

 

The actual experienced level of sulfur in bunker fuels is now around
2.7%, so the reduction isn't going to be a factor of 10.  And it will
require a significant effort on the part of refiners to achieve the
target levels, so some slippage is likely.  I also doubt that ships will
be equipped with high sulfur and low sulfur fuels, although some ships
that do mainly transoceanic routes like container ships may be given
waivers to use only high sulfur fuel in order to keep the aerosol levels
up.  At some point, however, the numbers work against such a bifurcated
system and low sulfur will prevail, the other fuel simply no longer
available in meaningful quantities.  

 

The reduction in negative forcing from tropospheric sulfate aerosols
will continue as Paul Crutzen predicted.  Not only will the contribution
from shipping eventually become negligible, but the same will be true
for coal and distillate fuels used on land and in air transportation.
All told, the loss of these aerosols may be as much as 1.6W/m2 by 2050
if not sooner.  The good news out of this besides the improvement in air
quality is that more sulfur in the form of H2S and SO2 will become
available for use in stratospheric aerosols if that approach is adopted.
Regardless, the real global warming is just getting started.


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[geo] Re: Televised debate

2009-05-03 Thread David Keith
David

 

While there is legitimate and sensible argument about how much warming
we might get from anthropogenic CO2, I think the overall physics and
atmospheric science linking anthropogenic CO2 emissions to the
expectation of increased warming is as solid as about anything in
science. The set of people who have actually rolled up their sleeves do
work serious work in atmospheric science and who also believe that there
is no connection between increased CO2 and warming is all but empty. Of
course, there are people who passionately believes there are aliens on
Air Force bases in Nevada, and likewise there are folks who have very
strong opinions about how the climate science is fundamentally wrong,
but I've yet to run into any of them who hold such opinions and actually
know the underlying science.

 

Do not over-read this statement. Of course, there are many thoughtful
scientists who think that the environmental risks posed by anthropogenic
climate change are overhyped (they often are), and also folks who
believe climate sensitivity will be on the lower end of the scale (it
may be).

 

Finally, your latter assertion is simply false. Discussion of the
concept of geoengineering arose in the 60's out of concern about CO2
driven climate change. See #26 at
www.ucalgary.ca/~keith/Geoengineering.html. The actual name arose in the
late 70s out of the same concern.

 

Yours,

David

 



From: geoengineering@googlegroups.com
[mailto:geoengineer...@googlegroups.com] On Behalf Of David Schnare
Sent: May 3, 2009 2:30 PM
To: kcalde...@globalecology.stanford.edu
Cc: ronald.da...@earthlink.net; ds...@yahoo.com; geoengineering
Subject: [geo] Re: Televised debate

 

Ken:

 

There is no argument about long-term global warming.  That warming, if
it continues, will justify geoengineering.  

 

There is, however, significant argument as to the causes of global
warming.  Indeed, there if far more valid, science-based argument made
by well respected university academics working specifically on the
issue, as to the causes of global warming, by far, than there is
argument over biological evolution or plate tectonics.  To characterize
the argument regarding the causes of global warming as in the same state
of knowledge as biological evolution or plate tectonics is not merely in
error, it is an unwelcome damper on legitimate research into these
phenomena.  

 

A public presentation on geoengineering need never address the causes of
global warming other than as necessary to discuss the physics of
management techniques.  Direct cooling efforts such as Solar Radiation
Management do not rest on the cause of global warming, only on the fact
of that warming.  Carbon sequestration techniques do presume a major
greenhouse gas component.  Any discussion of carbon sequestration
techniques should be conditioned on a clear statement of the
presumption.  Whether carbon is at the heart of the warming problem need
not be argued or discussed, other than for purposes of predicting the
likely degree of cooling expected from any particular geoengineering
technique.  

 

Finally, geoengineering rose out of a concern of a pending ice age, not
out of concern about any anthropogenic global warming.  Overall,
geoengineering is intended to be a large scale response to climate
change, whether human or natural.

 

David Schnare

On Sun, May 3, 2009 at 1:32 PM, Ken Caldeira
kcalde...@globalecology.stanford.edu wrote:

It is not a distraction. A good mechanistic understanding of causes of
change is essential.

If you do not understand the mechanisms behind global warming, how can
you sensibly intervene in the climate system? 

How can you simultaneously believe that (a) you can add a bunch of
radiatively active gases to the atmosphere and not affect climate and
(b) you understand how affecting Earth's radiation balance will affect
climate?

There is no argument about whether most global warming is
anthropogenic, just as there is no argument about whether there is
biological evolution or plate tectonics.





___
Ken Caldeira

Carnegie Institution Dept of Global Ecology
260 Panama Street, Stanford, CA 94305 USA

kcalde...@ciw.edu; kcalde...@stanford.edu
http://dge.stanford.edu/DGE/CIWDGE/labs/caldeiralab
+1 650 704 7212; fax: +1 650 462 5968   






On Sun, May 3, 2009 at 9:05 AM, Ron ronald.da...@earthlink.net wrote:


To some extent the whole argument about whether global warming is
anthropogenic is a distraction. Regardless of cause, understanding
global warming enough to counter it is more important. We may need to
rank possible solutions according to how fast and cheaply we can
implement them. We may need a two or three tier approach, implementing
the first tier to buy us enough time to do the next tier.

The vast changes in forest, ocean plants, combined with projected
increases in new coal fired power plants present a daunting challenge.
We will need to continuously 

[geo] Re: Televised debate

2009-05-03 Thread David Keith
I was just about to send links to the same.

 

The reason it's relevant, is that this undercuts the common claim that
concern about warming is recent and that atmospheric scientists in the
60s and 70s were mainly concerned about cooling. When you read the
relevant documents (that is the high-level synthesis reports that should
have been people's best shot at the science) the answer is the opposite,
folks were worried about warming due to CO2 for exactly the same reasons
they are now. We have fancier models, but the underlying physics is
still simple and convincing.

 

As in any case where a signal gradually sticks its head up above the
noise there's room to argue about exactly how much of the 20th century
warming is anthropogenic.

 

But it's not the 20th century warming, nor the correlation between CO2
concentrations and temperature that are the basis of concern. The
fundamental reason for concern is the same as it was when the report was
written for President Johnson. It was cooling then, but it was clear
that substantial increases in atmospheric CO2 would drive warming. We
know much more now, but the issue is the same. We are worried about the
consequences of a CO2 doubling or tripling under business as usual would
happen on a timescale approximately 10^5 times faster than the decline
in CO2 concentrations from the PETM to about 10 M years ago.

 

I think it's just nonsense to say that a discussion of geoengineering
need not be encumbered by this science. 

 

If this science was fundamentally flawed, as it would have to be if CO2
turns out not to be a major forcing, then there would be little basis
to trust the science that underlies the understanding of geoengineering.

 

Yours,

David

 

 

 

 

 

 



From: kcalde...@gmail.com [mailto:kcalde...@gmail.com] On Behalf Of Ken
Caldeira
Sent: May 3, 2009 10:29 PM
To: David Schnare
Cc: David Keith; ronald.da...@earthlink.net; ds...@yahoo.com;
geoengineering
Subject: Re: [geo] Re: Televised debate

 

The report to Johnson is available at:

http://dge.stanford.edu/DGE/CIWDGE/labs/caldeiralab/Caldeira_Research_ge
orefs.html

A direct link to the pdf is at:

http://dge.stanford.edu/DGE/CIWDGE/labs/caldeiralab/Caldeira%20downloads
/PSAC,%201965,%20Restoring%20the%20Quality%20of%20Our%20Environment.pdf

I attach jpegs of two relevant passages that make it clear that global
warming (not cooling) was the concern.






On Sun, May 3, 2009 at 5:45 PM, David Schnare dwschn...@gmail.com
wrote:

David:

 

I must rely on you for the history of geoengineering, that being one of
you academic interests and areas of expertise.  My reference to the
beginning of geoengineering was to the discussions in the Johnson White
House related to what then was thought likely to be global cooling, and
alternative means to mitigate such cooling.  I do not recall what folks
were saying would be the cause of such cooling, but I don't believe it
was CO2.

 

With regard to greenhouse gases and global warming, I did not state that
they had no forcing effect.  The argument is as to the size of their
role, and GHGs significance as compared to natural cycles.  That
argument is ongoing, and people who have actually rolled up their
sleeves do work serious work in atmospheric science include many who
discount CO2 as a major forcing.  That set is not empty, and if you want
a list, I can jin one up.  It would include former authors and lead
authors for the IPCC.  I do agree that those who believe there is no
connection between increased CO2 and warming are wrong.  I agree
because you used the phrase no connection.  The argument is about how
much connection there is.

Finally, you did not respond to my suggestion that for SRM related
approaches, it does not matter too much as to the GHG versus natural
cycles arguments.  SRM is a bandaid, not a cure.  Carbon sequestration,
on the other hand, is a cure, but only if GHG forcing is a significant
contributor to the forcing.  If, however, GHGs are not a large element
of warming, they remain a potentially large element of ocean
acidification, and thus carbon sequestration still remains an important
potential means to address a global problem.

 

Thus, a cogent discussion on geoengineering need not be encumbered by
arguments about causality of climate change.  Those seeking carbon
emissions reductions, include many of whom study geoengineering.  Those
folks do not wish to ignor, diminish or dispute the need for carbon
reduction.  Others interested in geoengineering, but not as concerned
about GHGs, are more agnostic on carbon reduction, but believe
geoengineering should not be used as a response to the AGW alarmists'
arguments.  Rather, they recognize the potential need for geoengineering
on other grounds, and simply discount the moral dilemma argument.

 

David Schnare.

 

On Sun, May 3, 2009 at 4:48 PM, David Keith ke...@ucalgary.ca wrote:

David

 

While there is legitimate and sensible argument about how

[geo] FW: McClean's article --geoengineering!

2009-04-27 Thread David Keith
Folks,

 

This is the most dramatic piece of hate mail I have yet received. The
only upside for a personal point of view is that he says i leave
vengence to God.

 

This one is interesting in linking chemtrails with HAARP and
illuminating the mixture with an apocalyptic strain of religious
fundamentalism.

 

The letter refers to the cover story on Canada's leading newsmagazine
which covered geoengineering:

 

http://www2.macleans.ca/2009/04/22/plan-b-for-global-warming/

 

Yours,

David

 

 



From: paul w [mailto:paulw...@yahoo.com] 
Sent: April 26, 2009 4:59 PM
To: David Keith
Subject: McClean's article --geoengineering!

 

Hello,

   After reading the article ,i cannot believe that you can lie like
this come on, thousands of people know that planes have been
spraying polymars,mold inhibiters,aluminum,barium and titanium which was
started in 1998 and it's called the SHIELD PROJECT by scientists and
CHEMTRAILS by the general publicSHAME how can you lie through your
teeth that you are just about to begin sprayingany idiot can look up
at the skies almost everywhere in the world and see planes intentionally
spraying these toxins into our atmosphere-how can you have studied
geoengineering all these years and not be aware than this GENOCIDE is
taking place and GENOCIDE it is because CHEMTRAILS are increasing
suicide rate amongst  people,killing the birds,bees ,trees,fish,changing
the texture of the snow and increasing severity of river floods and on
and on and on!--it is the most evil thing that has ever been
undertaken in the history of the human race and Yahweh Most High God is
going to punish you more severly than Hitler and Stalin combined,
forever and ever in the Lake of Fire where your worm will not die and
the fire is not quenched and God has a special flame for the
wicked!you must be another one of those who are insane from the
evolution lieeven the devils tremble before God you fools and God is
going to show you what you missed you disgustingly evil
scientists--and the fact that you keep lying to the public proves
that what you are doing is evil and God abhors liars worse than
murderers---i leave vengence to God but i have a feeling when the
godless masses find out that it's lying scientists causing climate
change with their H.A.A.R.P. Sites and chemtrails and other wicked
experiments ,the masses are going to go balistic like never before in
history-you don't even love your own children if you can lie like
you do for a living -if you want to know what the next 50 years of
hell are going to be like the study the Book of Revelation in the King
James Bible and i guarantee you that NOT ONE WORD will fail---around
2060 Yahshua the Messiah will return with 200,000,000, reaping angels
from the far end of Heaven and throw the wicked into the Lake of Fire
cannot break the Word of God so if you want to be in Yahweh's
beautiful Kingdom on a supernaturally renewed surface of earth where His
people will live in peace then start REPENTING OF YOUR LIES and EVIL
EXPERIMENTS---there will be much wailing and gnashing of teeth

 
sincerely 

 
Paul 

 

 --Satan has a short time--50 years!---CANNOT SAVE THE
EARTH2Peter3:10

 


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[geo] Re: EGU meeting, April 19-24

2009-04-21 Thread David Keith

Alan

You imply a geoengineered Pinatubo would reduce crop productivity in a
high-CO2 world. 

Can you provide some argument to support the case?

It's true that because of change in surface energy balance you reduce
precip more than temps, so that if temps are back to pre-industrial mean
the precip is down. 

But in a geoengineered climate, evaporation is also down. So is
precipitation variability. 

Total precip does not determine the outcome in any simple way.

My guess, supported by the studies with coupled ecosystem models, is
that solar shielding would increase crop productivity and NPP vs a
high-CO2 no-geo baseline. 

Of course, the effects would not be uniform.

Yours,
David




-Original Message-
From: geoengineering@googlegroups.com
[mailto:geoengineer...@googlegroups.com] On Behalf Of Alan Robock
Sent: April 21, 2009 6:54 AM
To: Ken Caldeira
Cc: j...@cloudworld.co.uk; geoengineering
Subject: [geo] Re: EGU meeting, April 19-24


Dear Ken,

If Mt. Pinatubo is the poster child, then this poster will contain 
drought in large parts of the world.  You can see the figures in the 
Trenberth and Dai (2007) GRL paper.  And don't forget, the effects of 
Pinatubo only lasted for a year.  A 1-year climate anomaly will not be 
that devastating, as food reserves and trade can compensate for 
agricultural shortfalls.  But a permanent aerosol cloud will make these 
effects last for decades.  So your poster, using Pinatubo as an example,

argues against geoengineering with stratospheric aerosols.

The ozone depletion from Pinatubo tells the same story, but I have not 
seen a study of how large the effects of that much enhanced UV would be 
on the ecosystem and humans.

I agree that the acid deposition would not seem to be a serious problem,

as we showed in our paper now under review at JGR.

Alan

Alan Robock, Professor II
   Director, Meteorology Undergraduate Program
   Associate Director, Center for Environmental Prediction
Department of Environmental SciencesPhone: +1-732-932-9800 x6222
Rutgers University  Fax: +1-732-932-8644
14 College Farm Road   E-mail: rob...@envsci.rutgers.edu
New Brunswick, NJ 08901-8551  USA  http://envsci.rutgers.edu/~robock


On Tue, 21 Apr 2009, Ken Caldeira wrote:

 For future sulfur emissions, see
 http://www.ipcc.ch/ipccreports/sres/emission/5-20.htm

 For past sulfur emissions, see the attached paper.

 Current sulfur emissions are on the order of 50 Tg/yr and for this
half
 century is likely to be in the range of 50 to 100 Tg/yr.

 The EGU abstract (
 http://meetingorganizer.copernicus.org/EGU2009/EGU2009-4831.pdf)
foresees
 emissions rates of 5 to 10 Tg/yr for the first half of the century,
which is
 roughly the 10% range of current emissions, with this percentage
scaling up
 if greenhouse gas concentrations continue to increase and tropospheric
 sulfur emissions decline.

 So, this is not negligible, but it is unlikely to be a game changer
either.

 It is my view that there would need to be some mighty compelling
reasons to
 deploy a stratospheric aerosol system, if not only because people who
 experience bad weather in subseuqent years might be incented to sue
(or even
 attack militarily) parties engaged in aerosol release.

 So, if we in an emergency situation acid rain, ozone loss, etc would
be
 among the costs taken into account before making a decision, but these
costs
 may not be decisive.

 I still think Mt Pinatubo is the poster child for stratospheric
aerosols
 approaches:  We know it can cool the Earth, we know it can do this
quickly,
 and we know it does not immediately cause a global catastrophe. Were
we
 faced with a real climate emergency, there could be a lot of pressure
to
 exercise the Pinatubo option. I do not see that the abstract by
Eliseev et
 al markedly changes this picture.

 Best,

 Ken
 ___
 Ken Caldeira

 Carnegie Institution Dept of Global Ecology
 260 Panama Street, Stanford, CA 94305 USA

 kcalde...@ciw.edu; kcalde...@stanford.edu
 http://dge.stanford.edu/DGE/CIWDGE/labs/caldeiralab
 +1 650 704 7212; fax: +1 650 462 5968



 On Mon, Apr 20, 2009 at 4:16 PM, John Nissen j...@cloudworld.co.uk
wrote:

  **
 *Some items from the EGU programme*
 **
 *Cryosphere - how much longer?*

 This should be an interesting session:
 http://meetingorganizer.copernicus.org/EGU2009/oral_programme/142

 Also on cryosphere is the session chaired by Peter Wadhams:
 http://meetingorganizer.copernicus.org/EGU2009/oral_programme/196

 And some potentially interesting presentations here:
 http://meetingorganizer.copernicus.org/EGU2009/oral_programme/702
 and here:
 http://meetingorganizer.copernicus.org/EGU2009/oral_programme/706

 *Geoengineering, session CL27*

 There seems to have been a disappointing response for this session.
 However the session does include a poster presentation from Russians
on
 SRM using stratospheric sulphur aerosols:
 

[geo] Re: a very simply way to lift sulfur

2009-03-24 Thread David Keith
1.  Space tethers are physics fun, but practical systems require
unobtainium. No materials are close to being strong enough to make them
interesting; indeed one can make an argument based on the strength of
chemical bonds that no such material is possible. 

 

2.  Tethered balloons are interesting. There are, however, lots of
engineering challenges in making a tether work at mid latitudes (in the
jet) and in making a tether that works as a hose.

 

 

3.  Aircraft are the default option. I am getting some work started
with a high-altitude aircraft engineering company on the topic. For the
lower and middle stratosphere this is likely to cheapest and most
controllable option. 

 

-David

 



From: geoengineering@googlegroups.com
[mailto:geoengineer...@googlegroups.com] On Behalf Of Albert Kallio
Sent: March 23, 2009 8:34 AM
To: agask...@nc.rr.com; Andrew Lockley
Cc: Geoengineering FIPC
Subject: [geo] Re: a very simply way to lift sulfur

 

The idea of space tethers is to pull up cable all the way to orbit and
then drive things to the geostationary orbit. I think it is far more
complex idea to this.
 
The throughput would have to be assessed correctly, the sharp attachment
point might be the issue with hose-blimp combinations due to turbulence,
just like tall buildings wave at winds the hose should be responding to
the air. But when weather is turbulent, supercells forming and winds
criss-crossing to all directions, then it would get entangled. 

But I would think that there are plenty of engineering solutions to keep
things floating orderly and managing any entanglement and the correct
trhoughput issue most surely.
 
Rgs,
 
albert
 



From: agask...@nc.rr.com
To: albert_kal...@hotmail.com; andrew.lock...@gmail.com
CC: geoengineering@googlegroups.com
Subject: [geo] Re: a very simply way to lift sulfur
Date: Mon, 23 Mar 2009 10:21:40 -0400

Such a tube would collapse under its own weight before getting more than
a few meters off the ground.  Also, a very thin tube wouldn't carry much
gas, so what's the point.  Winds near the tropopause would cause most
materials to break, including hoses attached to blimps.

- Original Message - 

From: Albert Kallio mailto:albert_kal...@hotmail.com  

To: Andrew Lockley mailto:andrew.lock...@gmail.com  ;
agask...@nc.rr.com 

Cc: Geoengineering FIPC mailto:geoengineering@googlegroups.com


Sent: Monday, March 23, 2009 9:30 AM

Subject: [geo] Re: a very simply way to lift sulfur

 

As per Andrews' suggestion below about nozzle up hydrogen, I
think it can become turbulent and vortexes form to dissipate and dilute
the gas. 
 
How about a very thin tubular plastic film that acts as a hose
to stand upright when filled by compressed hydrogen - sulphur mixture. 
 
The correct throughput ratios (pressures, diameter and mixture)
could be tested with short films and then the length of the film is
increased gradually to the right target altitude. 
 
As hydrogen is buoyant and the pressure is slighly higher gas
would keep more or less upright as long as there is gas fed into it at
the rate it is seeping out from the other end, plus any leakage in the
upward transmission in between (tube can deteriorate and leak). 
 
The diameter could be utilised to suit the flow. 
 
The hose would act like a long standing balloon, possibly snap
in severe weather but these could be looked at and nylon reinforcement
line perhaps attached to it.
 
I would try with first very short plastic film, then adding more
and more metres onto it. Ultimately, this should then go all the way up
modifying the top for different conditions.
 
Rgs, 
 
Albert

 





Date: Sun, 22 Mar 2009 17:52:42 +
Subject: [geo] Re: a very simply way to lift sulfur
From: andrew.lock...@gmail.com
To: agask...@nc.rr.com
CC: geoengineering@googlegroups.com

I think with correct design you could send up a large plume
successfully into the stratosphere.  High pressure gas should exit the
container or nozzle at high speed, forming a very wide column of fast
moving gas.  Heating the gas would help also.  This process is very
similar to the way volcanos work.  If you wanted to protect the ozone
layer, then adding ozone to the mix as suggested should make a
significant difference.


I'm thinking of something on the scale of the gas storage towers
you see in the UK, bursting open very suddenly.  This would require no
expensive balloons which yould turn to litter. As there was no equipment
or envelope to lift, a lower concentration of H2 lifter would be needed.

 

A

2009/3/22 Alvia Gaskill agask...@nc.rr.com

No it 

[geo] Re: Atmospheric 'Sunshade' Could Reduce Solar Power Generation

2009-03-24 Thread David Keith
 

On Thu, 19 Mar 2009, David Keith wrote:

 

 I think this issue is grossly overhyped

 

 

 

 1. It only matters for concentrating solar.

 

 

It matters much more for concentrating solar, but proposals for many new 

systems emphasize concentrating solar, because it is more efficient. 

Even for regular photovoltaic, the reductioun in sunlight would reduce 

solar power.

 

Concentrating solar is not necessarily more efficient. It may end up winning on 
capex, but it is far, far too early to call the winner. See our recent solar 
study from EST to give you a sense of the range of uncertainty judgment about 
the future cost declines in solar PV held by experts in PV development:

 

www.ucalgary.ca/~keith/Other Energy.html 
http://www.ucalgary.ca/~keith/Other%20Energy.html  (Paper #100).

 

-D

 

 

 

 2.  In a case for we really were in a bad enough state to be 

 geoengineering is not clear that the loss of solar output would be 

 that big a deal when you really balance the overall costs and risks.

 

Mitigation will need many different responses simultaneously, beginning 

now, and many more concentrated solar systems are being built now.  If 

at some point we do geoeengineering with scattered sunlight, we will 

have to do that much more to compensate for the loss of solar energy. 

So why plan two incompatible solutions to global warming?

 

Need to do the math here. Look at the model I presented in Copenhagen. I think 
we both view geo as something we do in a contingency where climate sensitivity 
turns out to be very high, not as a baseline plan. In that contingency, the GDP 
costs of climate damages are high. Compared to these costs the loss of a 
fraction of concentrating solar, which is itself a fraction of solar and even 
smaller fraction of primary energy would be a few % of the annualized 
mitigation costs, which under this scenario would be small compared to the 
damage costs. 

 

Are you suggesting that in a situation where climate damages were so severe 
that the benefits of geo outweighed the costs that one would not do geo just 
because of the loss of solar output?  I just don't see an argument here.  
Please be more specific about what specific consequences for decision-making is 
entailed by the possible loss of solar power output under some geo schemes. 

 

 

 

 3.  There are many geoengineering schemes that can avoid the forward 

 scattering problem, such as various engineered particles in the upper 

 atmosphere, or so it's by no means clear we would have this problem in 

 any case.

 

You say, this, but please provide the references for these many schemes. 

I know of theoretical speculation about making such particles, but no 

demonstration that they can be created with the proper characteristics 

on a massive scale nor that the fallout would be innocuous.  We know a 

lot about sulfate aerosols from volcanic eruptions, their benefits and 

problems, but what do we know about these many other schemes?

 

Of course there is no demonstration engineered particles can work. However, 
the physics that says you can make particles out of benign materials which do 
not have much forward scattering is old, simple and un-disputed.  I don't think 
there's any doubt you could fabricate such particles and put them in the 
atmosphere. I have a paper under review that outlines a particular method. But 
even if 10's of nice papers were published and there was a small demonstration 
we would still, of course, not have a demonstration that such a method would 
work at scale and that we would understand all the side effects.  The 
forthcoming Novim says a bit more about different kinds of particles and about 
a pathway for development and testing. Note that, while it's clear we know much 
more about sulfur we don't know for sure that sulfur particles of the relevant 
size can be efficiently maintained in the stratosphere, we also know many of 
the disadvantages of sulfur. It's far too early to really evaluate these 
options in a comparative way. That's why we need broad-based research program. 

 

 

 

 

 -David

 

 

 

 

 

 From: geoengineering@googlegroups.com 
 [mailto:geoengineer...@googlegroups.com] On Behalf Of Nick Woolf

 Sent: March 17, 2009 5:30 PM

 To: r...@llnl.gov; geoengineering@googlegroups.com; 
 climateintervent...@googlegroups.com

 Subject: [geo] Re: Atmospheric 'Sunshade' Could Reduce Solar Power Generation

 

 

 

 Dear All:

 

 The issue of the loss to solar concentrators is

 

 dependent on how much solar concentration is

 

 needed.

 

 

 

 Since silicon fails to match the cost of

 

 other power by a factor of 4, some higher

 

 concentration on it, e.g. by a factor 8 should do,

 

 provided that no more than half the cost is made

 

 up by auxiliary optics, steel etc.

 

 

 

 The angle of collection for an 8x concentrator

 

 is extremely wide, and would not be appreciably

 

 affected

[geo] Re: a very simply way to lift sulfur

2009-03-24 Thread David Keith
I completely agree that the focus should be on thing works without
producing too much acid rain or snow or other unanticipated negative
effects. That's where my focus is and I think the focus of most
research in the area.

 

-D

 

 



From: Eugene I. Gordon [mailto:euggor...@comcast.net] 
Sent: March 24, 2009 10:17 AM
To: David Keith; 'Geoengineering FIPC'
Subject: RE: [geo] Re: a very simply way to lift sulfur

 

Why isn't the focus on whether the thing works without producing too
much acid rain or snow or other unanticipated negative effects? If
viability is proven then problem #2 is cost of lifting. I would suggest
very strongly that problem #2 is solvable many different ways and I
would not waste too much time on it at this point. Whatever, the cost of
lifting in a practical implementation, having a proven technical
approach eliminates the naysayers and moves the discussion onto a more
practical level. Let us lift the technology before lifting the sulfur!

 



From: geoengineering@googlegroups.com
[mailto:geoengineer...@googlegroups.com] On Behalf Of David Keith
Sent: Tuesday, March 24, 2009 11:57 AM
To: Geoengineering FIPC
Subject: [geo] Re: a very simply way to lift sulfur

1.  Space tethers are physics fun, but practical systems require
unobtainium. No materials are close to being strong enough to make them
interesting; indeed one can make an argument based on the strength of
chemical bonds that no such material is possible. 

 

2.  Tethered balloons are interesting. There are, however, lots of
engineering challenges in making a tether work at mid latitudes (in the
jet) and in making a tether that works as a hose. 

 

 

3.  Aircraft are the default option. I am getting some work started
with a high-altitude aircraft engineering company on the topic. For the
lower and middle stratosphere this is likely to cheapest and most
controllable option. 

 

-David

 



From: geoengineering@googlegroups.com
[mailto:geoengineer...@googlegroups.com] On Behalf Of Albert Kallio
Sent: March 23, 2009 8:34 AM
To: agask...@nc.rr.com; Andrew Lockley
Cc: Geoengineering FIPC
Subject: [geo] Re: a very simply way to lift sulfur

 

The idea of space tethers is to pull up cable all the way to orbit and
then drive things to the geostationary orbit. I think it is far more
complex idea to this.
 
The throughput would have to be assessed correctly, the sharp attachment
point might be the issue with hose-blimp combinations due to turbulence,
just like tall buildings wave at winds the hose should be responding to
the air. But when weather is turbulent, supercells forming and winds
criss-crossing to all directions, then it would get entangled. 

But I would think that there are plenty of engineering solutions to keep
things floating orderly and managing any entanglement and the correct
trhoughput issue most surely.
 
Rgs,
 
albert
 



From: agask...@nc.rr.com
To: albert_kal...@hotmail.com; andrew.lock...@gmail.com
CC: geoengineering@googlegroups.com
Subject: [geo] Re: a very simply way to lift sulfur
Date: Mon, 23 Mar 2009 10:21:40 -0400

Such a tube would collapse under its own weight before getting more than
a few meters off the ground.  Also, a very thin tube wouldn't carry much
gas, so what's the point.  Winds near the tropopause would cause most
materials to break, including hoses attached to blimps.

- Original Message - 

From: Albert Kallio mailto:albert_kal...@hotmail.com  

To: Andrew Lockley mailto:andrew.lock...@gmail.com  ;
agask...@nc.rr.com 

Cc: Geoengineering FIPC mailto:geoengineering@googlegroups.com


Sent: Monday, March 23, 2009 9:30 AM

Subject: [geo] Re: a very simply way to lift sulfur

 

As per Andrews' suggestion below about nozzle up hydrogen, I
think it can become turbulent and vortexes form to dissipate and dilute
the gas. 
 
How about a very thin tubular plastic film that acts as a hose
to stand upright when filled by compressed hydrogen - sulphur mixture. 
 
The correct throughput ratios (pressures, diameter and mixture)
could be tested with short films and then the length of the film is
increased gradually to the right target altitude. 
 
As hydrogen is buoyant and the pressure is slighly higher gas
would keep more or less upright as long as there is gas fed into it at
the rate it is seeping out from the other end, plus any leakage in the
upward transmission in between (tube can deteriorate and leak). 
 
The diameter could be utilised to suit the flow. 
 
The hose would act like a long standing balloon, possibly snap
in severe weather but these could be looked at and nylon reinforcement
line perhaps attached to it.
 
I would try with first very short plastic film, then adding more

[geo] Re: Atmospheric 'Sunshade' Could Reduce Solar Power Generation

2009-03-19 Thread David Keith
I think this issue is grossly overhyped

 

1. It only matters for concentrating solar.

 

2. In a case for we really were in a bad enough state to be geoengineering 
is not clear that the loss of solar output would be that big a deal when you 
really balance the overall costs and risks.

 

3. There are many geoengineering schemes that can avoid the forward 
scattering problem, such as various engineered particles in the upper 
atmosphere, or so it's by no means clear we would have this problem in any case.

 

-David

 



From: geoengineering@googlegroups.com [mailto:geoengineer...@googlegroups.com] 
On Behalf Of Nick Woolf
Sent: March 17, 2009 5:30 PM
To: r...@llnl.gov; geoengineering@googlegroups.com; 
climateintervent...@googlegroups.com
Subject: [geo] Re: Atmospheric 'Sunshade' Could Reduce Solar Power Generation

 

Dear All:

The issue of the loss to solar concentrators is

dependent on how much solar concentration is 

needed.

 

Since silicon fails to match the cost of

other power by a factor of 4, some higher

concentration on it, e.g. by a factor 8 should do,

provided that no more than half the cost is made 

up by auxiliary optics, steel etc.

 

The angle of collection for an 8x concentrator

is extremely wide, and would not be appreciably

affected by forward scattering into a 45 degree 

cone.

 

Of course for those that want solar electricity

to fail, any stick is good enough to beat a dog.

 

Nick Woolf

- Original Message - 

From: Greg Rau mailto:r...@llnl.gov  

To: geoengineering@googlegroups.com ; 
climateintervent...@googlegroups.com 

Sent: Tuesday, March 17, 2009 2:02 PM

Subject: [geo] Atmospheric 'Sunshade' Could Reduce Solar Power 
Generation

 

 

http:// www. sciencedaily.com/releases/2009/03/090311124022.htm 
http://%20www.%20sciencedaily.com/releases/2009/03/090311124022.htm 

See Web-Photo:  The world's largest solar power facility, located near 
Kramer Junction, CA, consists of five Solar Electric Generating Stations and 
covers more than 1,000 acres. (Credit: Department of Energy/National Renewable 
Energy Laboratory)

 

Atmospheric 'Sunshade' Could Reduce Solar Power Generation

 

ScienceDaily (Mar. 16, 2009) - The concept of delaying global warming 
by adding particles into the upper atmosphere to cool the climate could 
unintentionally reduce peak electricity generated by large solar power plants 
by as much as one-fifth, according to a new NOAA study.

 Injecting particles into the stratosphere could have unintended 
consequences for one alternative energy source expected to play a role in the 
transition away from fossil fuels, said author Daniel Murphy, a scientist at 
NOAA's Earth System Research Laboratory in Boulder, Colorado.   The Earth is 
heating up as fossil-fuel burning produces carbon dioxide, the primary 
heat-trapping gas responsible for man-made climate change. To counteract the 
effect, some geoengineering proposals are designed to slow global warming by 
shading the Earth from sunlight.   Among the ideas being explored is injecting 
small particles into the upper atmosphere to produce a climate cooling similar 
to that of large volcanic eruptions, such as Mt. Pinatubo's in 1991. Airborne 
sulfur hovering in the stratosphere cooled the Earth for about two years 
following that eruption.

Murphy found that particles in the stratosphere reduce the amount and 
change the nature of the sunlight that strikes the Earth. Though a fraction of 
the incoming sunlight bounces back to space (the cooling effect), a much larger 
amount becomes diffuse, or scattered, light.   On average, for every watt of 
sunlight the particles reflect away from the Earth, another three watts of 
direct sunlight are converted to diffuse sunlight. Large power-generating solar 
plants that concentrate sunlight for maximum efficiency depend solely on direct 
sunlight and cannot use diffuse light.

Murphy verified his calculations using long-term NOAA observations of 
direct and diffuse sunlight before and after the 1991 eruption.  After the 
eruption of Mt. Pinatubo, peak power output of Solar Electric Generating 
Stations in California, the largest collective of solar power plants in the 
world, fell by up to 20 percent, even though the stratospheric particles from 
the eruption reduced total sunlight that year by less than 3 percent.   The 
sensitivity of concentrating solar systems to stratospheric particles may seem 
surprising, said Murphy. But because these systems use only direct sunlight, 
increasing stratospheric particles has a disproportionately large effect on 
them.

Nine Solar Electric Generating Stations operate in California and more 
are running or are under construction elsewhere in the world. In sunny 
locations such systems, which use curved mirrors or other