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: [email protected] [mailto:[email protected]] 
On Behalf Of Hawkins, Dave
Sent: Tuesday, May 01, 2012 10:51 AM
To: [email protected]; [email protected]
Cc: [email protected]
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: [email protected]<mailto:[email protected]> 
[mailto:[email protected]] On Behalf Of Nathan Currier
Sent: Tuesday, May 01, 2012 11:38 AM
To: [email protected]<mailto:[email protected]>
Cc: [email protected]<mailto:[email protected]>; 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 states, Penn and Ohio, would
be the most helpful, and in fact possibly even more useful *because* it's
in the troposphere, I feel. But it needs to be done very soon, as the new

CAIR program rules are apparently going to reduce all of this a good deal

more in the next 3-4 yrs, I believe.

All best,

Nathan

On Monday, April 30, 2012 2:44:33 PM UTC-4, David Hawkins wrote:

The largest insight I draw from this paper is the reminder that there are 
fairly large-scale activities going on right now that might provide useful 
information regarding SRM if we had systems set up to monitor resulting changes.

This paper documents one of them - the large reversal of sulfate loadings in 
the eastern half of the US, mostly occurring since the 1990 Clean Air Act was 
passed.  And those reductions will continue.  Rules promulgated by EPA in the

last six months will required millions of tons more of SO2 and NOx reductions 
over the next 3-5 years.

It would be nice to do a rapid assessment of what additional instrumentation 
might produce even more useful information, relevant to the many unanswered 
questions  about SRM.  To be sure, most of these reductions are

occurring in the troposphere and so may not be directly applicable to SRM in 
the stratosphere.  Still, I imagine there could be useful information to be 
gathered.  It might be much easier to get governments to devote some

money to such an enhanced measurement effort than to try to stand up some new 
"geoengineering program."







From: [email protected]<mailto:[email protected]> 
[mailto:[email protected]<mailto:[email protected]>]
 On Behalf Of Mike MacCracken
Sent: Sunday, April 29, 2012 8:38 PM
To: Geoengineering
Subject: Re: [geo] Regional SRM experiment



Hi David-Very interesting, and just why it might be possible to do something to 
limit warming in an area like the Arctic, which, as was documented over and 
over again at the Montreal IPY meeting last week, is changing very fast.

Mike MacCracken

********


On 4/28/12 10:06 AM, "David Hawkins" <MailScanner has detected a possible fraud 
attempt from "[email protected]" claiming to be 
[email protected]<http://[email protected]>> wrote:

Climatic effects of 1950-2050 changes in US anthropogenic aerosols - Part 2: 
Climate response
http://www.atmos-chem-phys.net/12/3349/2012/acp-12-3349-2012.pdf


Reduction in air pollution from coal fired power stations due to environmental 
regulations since the 1980s has increased regional global warming in the 
Central and Eastern United States. Climate scientists from the Harvard School 
of Engineering and Applied Sciences (SEAS) found that particulate pollution, 
particularly from coal fired power stations, caused a global warming hole, or a 
large cold patch reducing temperatures by up to 1 degree C in the region, 
particularly lowering maximum temperatures in Summer and Autumn.


Since I have spent a good deal of the past several decades advocating for rapid 
deployment of particle reducing techniques, I guess I can be tagged as an 
inadvertent geoengineer.
:>)

Sent from my iPad

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