If the documented history of the Earth's climate for the past 450 million
years (see www.scotese.com) has any relevance, the global average
temperature is headed for 25 C, up almost 10 degrees C from current values,
even without the benefit of anthropogenic CO2. Needless to say, but worth
emphasizing, even if we stopped producing CO2 tomorrow and could remove
current excess atmospheric values we are headed for serious climate warming
problems. The social implications are enormous and there is little doubt
that techniques for minimizing the temperature rise will become essential if
they are not now extremely important. Hence I argue for formalizing the
study of geoengineering techniques/technology before leaping in to do
something about current concerns with a particular approach. Having a formal
geoengineering society would have immense value. Plant some of the seed.
Don't simply eat it all now.

-----Original Message-----
From: [email protected]
[mailto:[email protected]] On Behalf Of Mike MacCracken
Sent: Tuesday, April 19, 2011 12:00 AM
To: Geoengineering
Subject: [geo] On what research I would suggest

Ken et al.--Note that I am going to focus on SRM approaches here. A word,
however, on CDR, which, it seems to me, is just not at all likely to make an
important contribution to limiting climate change until global emissions are
brought down a good bit through efficiency, essentially giving up coal, etc.
With global C emissions nearing 10 GtC/yr and rising, working on approaches
that at maximum might make it up to sequestering 1-2 GtC/yr is just
premature--we need to take other steps first. The one exception here, it
seems to me, is to see if we can figure out how to deal with ocean
acidification such as through Greg Rau's approach--I'm not sure if that is
more mitigation or not.

On SRM approaches, as I have been saying for a couple of years, it seems to
me that the highest priority for early research should be on determining if
it is possible to use various of the proposed SRM techniques in very focused
ways to limit worsening impacts in the near-term (in places like the Arctic,
the loss of sea ice, ice sheet mass, and permafrost is an emergency now, or
nearly so, and so waiting to move toward implementation seems too hesitant
to me. With this perspective, I would set up a very mission-focused program
goal of coming up with a tested approach for dealing with one or more of the
most severe impacts, aiming for making a decision to move forward with
implementation starting in of order of five years (so a 5-year research
program to get to the implementation stage, and then ongoing research as
implementation is in progress).

The types of impacts that I would choose to focus on would include some
combination of the following (and there are of course interlinkages):
generally reducing Arctic warming (which would also lead to some likely
beneficial cooling in mid-latitudes); slowing the loss of ice from the major
ice sheets; keeping permafrost frozen; redirecting or intensifying seasonal
storm tracks into increasingly arid regions like southwestern North America
and/or Australia; cooling the waters where hurricanes/tropical cyclones
intensify; and similar steps. There are those who argue that nothing can be
done primarily regionally--that everything leads to global responses;
determining whether such global connections are statistically significant or
not (and whether varying details of the implementation could be done to
reduce them) would be a clear issue to research--including whether what
long-distant linkages there are are beneficial or harmful.

With focused objectives such as these, I would think that there could be
much more focused environmental and social science research as well--much
more clearly presenting the issue as a risk-risk evaluation than arises in
discussions of future global geoengineering. On the benefit side there would
at least be a clear beneficial change being sought, which can get much more
confused in the global case. I should also note that I think focusing on
moderating regional-scale impacts, there would hopefully be less of a
tendency to reduce effort on mitigation (if that really is a problem),
because, of course, there are a whole host of impacts not being addressed.

Not only would success in coming up with an approach for dealing with severe
impacts such as mentioned above, but it would also help to build
understanding about the various approaches and the basis for ongoing, but
lower priority research on potential global implementation, which I think
should also be considering what I think would be more realistic
implementation scenarios (e.g., implementing incrementally to stop and
slowly reduce radiative forcing starting in the near-term) than imagining
we'd figure out and agree on when some threshold has been passed and do a
large and sudden emergency implementation (not even being clear that when so
far along everything can be reversed).

I've written up some of these ideas over the past year or too for various
studies, but had not passed them around, so will attach to this message. The
first memo offers some thoughts on how I would organize a US program, and an
accompanying table suggest some specific research efforts. Note that this
memo envisions not just the very focused applied effort, but also an
independent research and evaluation effort to keep make sure questions get
raised and considered--again relating to moving toward the specific proposed
objective, but in this effort on real and potential shortcomings, and not
just a general research effort (we need more money for that). The second
memo was prepared as a more detailed example of how one might structure the
component of the program aimed at moving rapidly to limit Arctic warming. It
is posed as a letter dated a few years hence seeking approval for moving
ahead with a major field program to test approaches that have already been
tested in computer simulations, etc. Clearly an optimistic timetable, but
really the type of one that is needed given what seem to be irreversible
changes (like loss of mass from Greenland, loss of biodiversity, etc.) that
we seem headed toward.

Note that the ideas written up are over a year old, so a bit dated. And
these are just ideas--they would greatly benefit from some intense
discussion about how to do even better, etc. I just think we are moving far
too slowly right now.

Best, Mike MacCracken



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