[geo] Re: New WMO Report on Weather Mod Plus Geoengineering

2013-08-22 Thread Jim Lee
I just have to say, I told you so

   - 
   https://groups.google.com/forum/#!msg/geoengineering/GfMt-0jXzDY/amVJ-V1vXQEJ
   - https://groups.google.com/d/msg/geoengineering/JFmkKOWe_wY/dbiJemslrqoJ

*It was also stated that if we still do not understand (Weather 
 Modification) at small scales (after 60 years), understanding what the 
 impacts of Geoengineering would be at large/global scale, should be seen as 
 a major challenge. 
 [1]http://www.wmo.int/pages/prog/arep/wwrp/new/documents/Doc_3_6_weather_mod_2013_Final_tn.pdf
 *


~ Jim Lee
http://climateviewer.com/geoengineering-weather-control.html



On Tuesday, August 20, 2013 7:45:57 AM UTC-4, Josh Horton wrote:

 This may interest some of you - a recent (brief) WMO report on weather 
 modification including some discussion of GE.


 http://www.wmo.int/pages/prog/arep/wwrp/new/documents/Doc_3_6_weather_mod_2013_Final_tn.pdf

 Josh


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[geo] ACP - Abstract - Self-limited uptake of α-pinene oxide to acidic aerosol: the effects of liquid-liquid phase separation and implications for the formation of secondary organic aerosol and organo

2013-08-22 Thread Andrew Lockley
http://www.atmos-chem-phys.net/13/8255/2013/acp-13-8255-2013.html

Self-limited uptake of α-pinene oxide to acidic aerosol: the effects of
liquid-liquid phase separation and implications for the formation of
secondary organic aerosol and organosulfates from epoxides

G. T. Drozd, J. L. Woo, and V. F. McNeillDepartment of Chemical
Engineering, Columbia University, New York, NY, 10027, USA

Abstract.
The reactive uptake of α-pinene oxide (αPO) to acidic sulfate aerosol was
studied under humid conditions in order to gain insight into the effects of
liquid-liquid phase separation on aerosol heterogeneous chemistry and to
elucidate further the formation of secondary organic aerosol and
organosulfates from epoxides. A continuous flow environmental chamber was
used to monitor changes in diameter of monodisperse, deliquesced, acidic
sulfate particles exposed to αPO at 25% and 50% RH (relative humidity). In
order to induce phase separation and probe potential limits to particle
growth from acidic uptake, αPO was introduced over a wide range of
concentrations, from 200 ppb to 5 ppm. Uptake was observed to be highly
dependent on initial aerosol pH. Significant uptake of αPO to aerosol was
observed with initial pH  0. When exposed to 200 ppb αPO, aerosol with pH
= -0.5 showed 23% growth, and 6% volume growth was observed at pH = 0.
Aerosol with pH = 1 showed no growth. The extreme acidity required for
efficient αPO uptake suggests that this chemistry is typically not a major
route to formation of aerosol mass or organosulfates in the atmosphere.
Effective partition coefficients (Kp, eff) were in the range of (0.1-2) x
10-4 m3μg-1 and were correlated to initial particle acidity and particle
organic content; particles with higher organic content had lower partition
coefficients. Effective uptake coefficients (γeff) ranged from 0.1 to 1.1 x
10-4 and are much lower than recently reported for uptake to bulk
solutions. In experiments in which αPO was added to bulk H2SO4 solutions,
phase separation was observed for mass loadings similar to those observed
with particles, and product distributions were dependent on acid
concentration. Liquid-liquid phase separation in bulk experiments, along
with our observations of decreased uptake to particles with the largest
growth factors, suggests an organic coating forms upon uptake to particles,
limiting reactive uptake.

Citation:
Drozd, G. T., Woo, J. L., and McNeill, V. F.: Self-limited uptake of
α-pinene oxide to acidic aerosol: the effects of liquid-liquid phase
separation and implications for the formation of secondary organic aerosol
and organosulfates from epoxides, Atmos. Chem. Phys., 13, 8255-8263,
doi:10.5194/acp-13-8255-2013, 2013.

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[geo] Attribution of 2012 US drought, application to geoengineering

2013-08-22 Thread Andrew Lockley
Poster's note : the paper below is interesting for general reading on AGW.
I also think it's particularly applicable to geoengineering governance,
because of the shift in public attitudes in the US which accompanied the
drought. From my limited and unscientific perspective on US public opinion,
the drought was accompanied by a drop in denialism. This matters for
geoengineering, because political attribution of extreme weather to AGW is
different from scientific attribution. Accordingly, pressure to geoengineer
may be largely unrelated to the science behind the immediate, purported
cause of this change in attitudes. Likewise, hostility to geoengineering
programmes may be entirely unconnected with the actual effects of these
programmes.

http://journals.ametsoc.org/doi/abs/10.1175/BAMS-D-13-00055.1

Causes and Predictability of the 2012 Great Plains Drought

M. Hoerling 1, J. Eischeid 2, A. Kumar 3, R. Leung 4, A. Mariotti 5, K.
Mo 3, S. Schubert 6, and R. Seager 7[...]
Bulletin of the American Meteorological Society

DOI: 10.1175/BAMS-D-13-00055.1
Abstract
Central Great Plains precipitation deficits during May-August 2012 were the
most severe since at least 1895, eclipsing the Dust Bowl summers of 1934
and 1936. Drought developed suddenly in May, following near-normal
precipitation during winter and early spring. Its proximate causes were a
reduction in atmospheric moisture transport into the Great Plains from the
Gulf of Mexico. Processes that generally provide air mass lift and
condensation were mostly absent, including a lack of frontal cyclones in
late spring followed by suppressed deep convection in summer owing to
large-scale subsidence and atmospheric stabilization.Seasonal forecasts did
not predict the summer 2012 central Great Plains drought development, which
therefore arrived without early warning. Climate simulations and empirical
analysis suggest that ocean surface temperatures together with changes in
greenhouse gases did not induce a substantial reduction in summertime
precipitation over the central Great Plains during 2012. Yet, diagnosis of
the retrospective climate simulations also reveals a regime shift toward
warmer and drier summertime Great Plains conditions during the recent
decade, most probably due to natural decadal variability. As a consequence,
the probability for severe summer Great Plains drought may have increased
in the last decade compared to the 1980s and 1990s, and the so-called
tail-risk for severe drought may have been heightened in summer 2012. Such
an extreme drought event was nonetheless still found to be a rare
occurrence within the spread of 2012 climate model simulations.
Implications of this study’s findings for U.S. seasonal drought forecasting
are discussed.

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Re: [geo] Governance of Geoengineering – A personal view

2013-08-22 Thread Oliver Tickell
I think the characterisation of Germany's Energiewende as a regression 
to fossil fuelled energy system is both cheap and wrong. Yes, they are 
closing nuclear power stations, but they are also making a huge shift of 
truly global significance to renewables and in the process creating a 
model of how to do it, that other countries will surely follow. Coal 
burning in the power sector has increased across Europe, but not because 
of nuclear closures. The main reason is that coal prices are very low 
(thanks in part to US switch to shale gas in power sector so much of 
their coal is now exported) while the EUETS carbon price has collapsed. 
Coal burning in Europe has increased to the detriment of much more 
expensive gas.


I note that your paper is for African Academy of Sciences. Surely all 
the more important for African audience to stress the importance of a 
switch to renewable energy, solar in particular, especially as huge coal 
burning projects in southern Africa are getting off the ground with 
ruinous consequences for climate.


Oliver.

On 21/08/2013 22:31, Andrew Lockley wrote:


This is a draft article I wrote for the African Academy of Sciences. 
I'd really appreciate any comments on it - before I irrecoverably 
embarrass myself!


Thanks

A

---

Governance of Geoengineering – A personal view

Climate change is here to stay.  That much is certain.  Due to the 
heat capacity of the oceans, we always feel the effect of emissions 
past.  Meanwhile, not only do emissions continue, but there’s still a 
breakneck rush to build carbon-spewing plant and vehicles.  This is 
true not only in the developing world, but also in affluent countries 
that are switching back to fossil – such as Germany, which has turned 
against nuclear. So not only are we bracing ourselves for the climate 
change that’s already in the mail, we’re also wilfully accelerating 
the process.
But it gets worse.  As emissions are cleaned up in the developing 
world, the aerosol haze which mutes global warming will fade away – 
exposing us to the full glare of a changing climate.  Furthermore, we 
are potentially exposed to major tipping points in the Earth’s climate 
system, such as the postulated release of methane in the Arctic.  Even 
in the unlikely event that we manage to rapidly decarbonise the 
economy, we may still find find that any intervention is too little, 
too late.
As a technology, geoengineering – and specifically solar radiation 
management -  is also here to stay.  We know we can do it.  We know we 
can do it fairly cheaply - certainly much more cheaply than rapid, 
large-scale mitigation.  We also know that it will work, albeit 
imperfectly, in reducing the impacts of climate change.  So what to do 
with this terrifyingly powerful technology?  We must bear in mind two 
facts.  Firstly, we are still emitting.  Secondly, even if we stop 
emitting there is at least a chance the climate is already in a 
dangerously unstable state.  Faced with a position like that, it’s 
hard to argue that we shouldn’t at least explore geoengineering 
technology.  And we’d be exploring for a very good reason:  committing 
to NOT geoengineering is rapidly beginning to look like a very 
dangerous idea indeed.
Beyond exploring, what could deployment actually look like? Well 
here’s the problem: the real world is a messy, dirty place.  We live 
in a world which tolerates reckless emissions, and much more besides.  
Protectionism, warfare, human rights abuses, genocide.  These are all 
ugly things that go on and the world tolerates them, to a greater or 
lesser extent.  We don’t have an effective global governance policy 
for such things, although we do try sometimes.  We have treaties, 
which are optional.  We have resolutions, which are ignored.  We have 
sanctions, which are ineffective.  And we have bombs, which yield 
highly unpredictable outcomes, and are more effective as a threat than 
as an intervention.  None of the above is terribly efficient at 
getting people or countries to behave themselves. So why do we pretend 
geoengineering will really be ‘governed’ by anything, or anyone?
My argument is that it won’t be governed at all.  Or at least, there 
isn’t any reason to assume that there will be a single, overall 
framework of governance that delivers an effective policy – regardless 
of whom that single, effective policy favours.
Could we not image a world where a chaotic muddle of overlapping and 
competing geoengineering schemes exists?  Take for example, a 
situation where a power bloc determines a policy of minimal 
intervention, but is overruled by a private carbon offset firm who 
offer to ‘top up’ the intervention.  This seems superficially 
possible, if not necessarily plausible.  Or perhaps a top up scheme 
could be provided by a nation state looking to preserve its glaciers?  
This top up could be provided in defiance of a state looking for a 
‘light touch’ geoengineering scheme, which allows it to open up 

RE: [geo] Re: New WMO Report on Weather Mod Plus Geoengineering

2013-08-22 Thread Doug MacMartin
Of course.  By the exact same logic, no-one understood combustion enough to
build an internal combustion engine until quantum mechanics was worked out.


 

Sorry, I don't see any connection at all between the ability to understand
small scale (in space and time) and the average of that behaviour over large
scales.  Statistical mechanics is a great example where the large scale is
quite predictable without requiring understanding of small scales.  While I
do agree with the conclusion that understanding the impacts is a challenge,
I don't think that the appeal to the failure of weather modification is
relevant.

 

d

 

From: geoengineering@googlegroups.com
[mailto:geoengineering@googlegroups.com] On Behalf Of Jim Lee
Sent: Wednesday, August 21, 2013 9:21 PM
To: geoengineering@googlegroups.com
Subject: [geo] Re: New WMO Report on Weather Mod Plus Geoengineering

 

I just have to say, I told you so

*
https://groups.google.com/forum/#!msg/geoengineering/GfMt-0jXzDY/amVJ-V1vXQE
J
*
https://groups.google.com/d/msg/geoengineering/JFmkKOWe_wY/dbiJemslrqoJ

It was also stated that if we still do not understand (Weather
Modification) at small scales (after 60 years), understanding what the
impacts of Geoengineering would be at large/global scale, should be seen as
a major challenge. [1]
http://www.wmo.int/pages/prog/arep/wwrp/new/documents/Doc_3_6_weather_mod_2
013_Final_tn.pdf 

 

~ Jim Lee

http://climateviewer.com/geoengineering-weather-control.html

 

 


On Tuesday, August 20, 2013 7:45:57 AM UTC-4, Josh Horton wrote:

This may interest some of you - a recent (brief) WMO report on weather
modification including some discussion of GE.

 

http://www.wmo.int/pages/prog/arep/wwrp/new/documents/Doc_3_6_weather_mod_20
13_Final_tn.pdf

 

Josh

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Re: [geo] New article on non-anthropogenic ocean fertilization in MEPS

2013-08-22 Thread Oliver Tickell
Thanks - useful papers. I did not know about Olaf's paper looking at 
spreading olivine sand on dynamic areas of seabed. I prefer his approach 
of letting the movement of the sea do the grinding for you, rather than 
using 30% of the C gain to grind the olivine to a fine powder using 
fossil energy. But one way this approach could make sense is, when solar 
PV gets even cheaper than it is now, to use solar electricity to do the 
grinding so there is very little carbon debt. Also it is interesting to 
know that dispersal of 1um olivine powder by commercial shipping could 
provide an appropriate amount of carbon drawdown to offset current 
emissions. This something that environmentally responsible shipping 
companies should consider, at least on a scale to offset their own 
emissions.


Oliver.

On 21/08/2013 19:11, Rau, Greg wrote:
If one is interested in silicate addition to the ocean (both for 
direct chemical and indirect bio effects on C), then I refer you to 
these links and refs therein:

http://m.iopscience.iop.org/1748-9326/8/1/014009/pdf/1748-9326_8_1_014009.pdf
http://www.earth-syst-dynam-discuss.net/2/551/2011/esdd-2-551-2011.pdf

Lots more silicate minerals around than just ash, and yes potential 
for positive (and negative) cation and anions effects on bio C, but 
lets find out.

Greg

From: Oliver Tickell oliver.tick...@kyoto2.org 
mailto:oliver.tick...@kyoto2.org

Organization: Kyoto2
Reply-To: oliver.tick...@kyoto2.org 
mailto:oliver.tick...@kyoto2.org oliver.tick...@kyoto2.org 
mailto:oliver.tick...@kyoto2.org

Date: Wednesday, August 21, 2013 7:59 AM
To: geoengineering geoengineering@googlegroups.com 
mailto:geoengineering@googlegroups.com
Subject: Re: [geo] New article on non-anthropogenic ocean 
fertilization in MEPS


Thanks! My last sentence should have read And of course the other 
question is re the chemical composition of the silicate in the ash and 
its particle size as this will determine its quality as a source of 
silicic acid. So you understood.


the rate of weathering is proportionate to surface area so small 
particles are hugely more effective at releasing silicic acid than 
large ones. Olivine grain sizes of 0.1mm are proposed for terrestrial 
application and far smaller than this (~ micrometre scale) for marine 
use so that the particles can weather during their residence in the 
water column. The 'powdery' fraction of the ash will give the greatest 
silicic acid contribution.


It's hard for me to comment further without seeing the paper but it's 
good to know that these questions have been considered, Oliver.


On 21/08/2013 15:05, Chris Vivian wrote:

Oliver,
Bear in mind that the North East Pacific is a high-nutrient, 
low-chlorophyll (HNLC) area that is known to be limited by iron. The 
paper gives estimated sea water concentrations of silicate in the 
North East Pacific in the top 20 metre mixed layer in August 2008 
when the volcanic eruption occurred of 5,000-15,000 nM (nana molar) 
compared to an estimated 6-20 nM supply from the ash fallout over the 
fertilized area in the Gulf of Alaska.
Your second point was unclear but I assumed you were querying the 
release rate of the silicate from the ash. The ash used in the 
experiment was collected on a fishing boat during the eruption and 
stored dry in containers. The experiment only used the  2 mm size 
fraction. The release rate of silicate in the experiments was 170 
nmol silicate per gram of ash in the first hour and up to 585 nmol 
silicate per gram of ash after 20 hours.

Chris.

On Wednesday, August 21, 2013 10:12:19 AM UTC+1, Oliver Tickell wrote:


IMHO the significance of the silicic acid would depend on the
time of year. In the spring silicic acid is generally abundant so
adding more of it would make little difference. One it has all
been used up and diatoms are giving way to other phytoplankton a
boost of silicic acid would give rise to a second diatom bloom -
so it would be very significant. And of course the other question
is how effectively the chemical composition of the silicate in
the ash and its particle size as this will determine its quality
as a source of silicic acid.

Have the authors given any serious examination to such questions?
Oliver.

On 21/08/2013 09:55, Chris Vivian wrote:

Oliver,
ï¿1Ž2
I have seen the paper but cannot post a copy online. In the
paper the authors did measure the release of nitrate, nitrite,
ammonia, phosphate and silicate in leaching experiments and
concluded that the impact of these macronutrients released from
Kasatochi ash on primary productivity was probably
minimal.ï¿1Ž2They also suggested that the release of trace
metals other than iron could also have influenced phytoplankton
growth.

ï¿1Ž2

Chris.
ï¿1Ž2
On Monday, August 19, 2013 4:23:59 PM UTC+1, Oliver Tickell wrote:

I have not found an open source version of this paper yet,
but here is 

RE: [geo] Re: New WMO Report on Weather Mod Plus Geoengineering

2013-08-22 Thread George Collins






   Of course.  By the exact same logic, no-one understood combustion enough to 
build an internal combustion engine until quantum mechanics was worked out. 
I worry that this exaggerates in at least two ways.
   I don’t see any connection at all between the ability to understand small 
scale (in space and time) and the average of that behaviour over large scales.
1. The small scale discussed in the report is tens of orders of magnitude 
closer to large scale than in your example. The world's smallest internal 
combustion engine (circa 2001) [*1] was about the size of a penny, which (at 
19.05mm) is around 1.18*10^33 times greater than Planck length; the area of the 
atmosphere is only about 31.8 million (3.18*10^7) times greater than the patch 
of sky over the WMO's home town of Geneva (and only about 12,000 times greater 
than the sky over Switzerland.) Might not the logic change if the scale 
difference is 37 septillion (~37,100,000,000,000,000,000,000,000) times less 
extreme?
   Statistical mechanics is a great example where the large scale is quite 
predictable without requiring understanding of small scales.
2. Then you have the question of whether city-scale atmosphere averages into 
global atmosphere the way that quantum particles average into solid objects, or 
statistically modeled particles average into idealized gases. My understanding 
(not having studied quantum mechanics formally in some years) is that quantum 
effects at mesoscale have to be carefully teased out because, inter alia, the 
small-scale effects typically average themselves away [Fermi-Dirac/binomial 
distribution of spins, etc *2]. But one look at a Hadley cell makes it clear 
that global atmosphere isn't a flat mean of local atmosphere. I'm not even sure 
that statistical mechanics works that well for you here--isn't turbulence 
theory a core area of research at both small and large scales?
And there are other problems (an engine, as a black box, is highly bounded with 
near-perfect observation of inputs and outputs, so control without low-level 
understanding is more plausible; in the atmospheric case, we're literally 
underneath the box and observing bits of it from above and below).
Anyway, not sure the WMO's point is that easy to dismiss...
*1 http://www.berkeley.edu/news/media/releases/2001/04/02_engin.html*2 
http://arxiv.org/ftp/physics/papers/0407/0407081.pdf
From: macma...@cds.caltech.edu
To: rez...@gmail.com
CC: geoengineering@googlegroups.com
Subject: RE: [geo] Re: New WMO Report on Weather Mod Plus Geoengineering
Date: Thu, 22 Aug 2013 07:38:24 -0700

 Of course.  By the exact same logic, no-one understood combustion enough to 
build an internal combustion engine until quantum mechanics was worked out.  
Sorry, I don’t see any connection at all between the ability to understand 
small scale (in space and time) and the average of that behaviour over large 
scales.  Statistical mechanics is a great example where the large scale is 
quite predictable without requiring understanding of small scales.  While I do 
agree with the conclusion that understanding the impacts is a challenge, I 
don’t think that the appeal to the failure of weather modification is relevant. 
d From: geoengineering@googlegroups.com 
[mailto:geoengineering@googlegroups.com] On Behalf Of Jim Lee
Sent: Wednesday, August 21, 2013 9:21 PM
To: geoengineering@googlegroups.com
Subject: [geo] Re: New WMO Report on Weather Mod Plus Geoengineering I just 
have to say, I told you 
sohttps://groups.google.com/forum/#!msg/geoengineering/GfMt-0jXzDY/amVJ-V1vXQEJhttps://groups.google.com/d/msg/geoengineering/JFmkKOWe_wY/dbiJemslrqoJIt
 was also stated that if we still do not understand (Weather Modification) at 
small scales (after 60 years), understanding what the impacts of Geoengineering 
would be at large/global scale, should be seen as a major challenge. [1] ~ Jim 
Leehttp://climateviewer.com/geoengineering-weather-control.html  
On Tuesday, August 20, 2013 7:45:57 AM UTC-4, Josh Horton wrote:This may 
interest some of you - a recent (brief) WMO report on weather modification 
including some discussion of GE. 
http://www.wmo.int/pages/prog/arep/wwrp/new/documents/Doc_3_6_weather_mod_2013_Final_tn.pdf
 Josh-- 
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