Gene:

You say the paleoclimate record tells us that the Earth will flip into a
warm state - increasing its average temperature by almost 10 degrees C from
current values? - without GHGs no less!  Please connect the dots for me/us
on how you arrived at this bold interpretation of the data.  Dr. Scotese's
website doesn't seem to offer this projection.  I would have thought the
paleoclimate record suggests a return to another glacial epoch - if we were
to ignore the effect of GHGs.  So when is your GHG independent warming going
to happen?  Within the next few decades I presume - clearly this is what you
suggest if we need a geoengineering society established now to deal with it.

Glyn

On Tue, Apr 19, 2011 at 6:11 AM, Eugene I. Gordon <[email protected]>wrote:

> 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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