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_d
ata_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]] On Behalf Of Nathan Currier
Sent: Tuesday, May 01, 2012 11:38 AM
To: [email protected]
Cc: [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]] 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" <[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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