Andrew

A few comments in response to this and the subsequent comment by

1. This vector representation is useful way to think about trade-offs when the 
climate response to CO2 and SRM is reasonably linear. This stuff is published 
as: Juan Moreno-Cruz, Katharine Ricke and David W. Keith. (2011). A simple 
model to account for regional inequalities in the effectiveness of solar 
radiation management. Climatic Change, doi: 10.1007/s10584-011-0103-z. 
(PDF)<http://www.keith.seas.harvard.edu/papers/131.Moreno-Cruz.Inequality.SRM.e.pdf>.
 Despite the hype about nonlinearity, models are quite linear in the region of 
interest, see the appendix to the paper.

2. I was surprised by our results. I expected the trade-offs to be much 
stronger. Doing this work pushed me to realize that SRM can do a substantially 
better job of compensating CO2-driven climate change than I had expected. (Of 
course, it does nothing about the geochemical impacts of CO2 such as ocean 
acidification.)

3. Yes, you can consider quantities other than temperature and precip; and 
quantities like soil moisture are certainly important.

4. Stephen Salter imply that these results were somehow particular to 
stratospheric sulfates, saying: I think that you must be referring to 
geo-engineering with stratospheric sulphur. With tropospheric salt you can vary 
precipitation in both directions by choosing the time and place to spray. This 
analysis is applicable to both. It is certainly true that if sea salt aerosol 
can be effectively used to alter cloud albedo over large areas--a proposition 
which is still quite uncertain--then it could be used to reduce (them 
eliminate) the trade-offs.

We looked at exactly this in a more recent paper examining how trade-offs can 
be reduced if you were able to adjust the intensity of SRM forcing at different 
locations in seasons:  Douglas G. MacMartin, David W. Keith, Ben Kravitz, and 
Ken Caldeira. (2012). Managing tradeoffs in geoengineering through optimal 
choice of non-uniform radiative forcing. Nature Climate Change, doi: 
10.1038/NCLIMATE1722. 
(PDF<http://www.keith.seas.harvard.edu/preprints/158.MacMartin.etal.ManagingTradeoffsThroughNonRadForc.p.pdf>).

Note that this paper explicitly looks at something people in this blog often 
ask about which is the ability to tune SRM to focus on restoring Arctic sea ice.

5. Finally, I do not understand your argument about soil moisture. Evaporation 
always equals precipitation the global mean. All else equal-- and it probably 
will not be--one expects variability to go down (not up) as you weaken the 
hydrological cycle. So my back of the envelope physics points the opposite way 
to yours. We look at this in one of the papers with Kate Ricke and found that 
at least the one case we looked at variability did go down.

Of course, model do not equal reality.

Yours,
David




From: geoengineering@googlegroups.com [mailto:geoengineering@googlegroups.com] 
On Behalf Of Andrew Lockley
Sent: Monday, November 26, 2012 7:08 AM
To: David Keith; geoengineering
Subject: [geo] Your Vector diagram


David

I remember the excellent vector diagram lecture you gave at Oxford.  In it you 
represented temperature and precipitation on a vector.diagram and showed that 
both cannot be simultaneously corrected exactly by geoengineering, but that the 
mismatch was small.

However, that would leave us in a world which was either slightly drier or 
slightly warmer than in a non-geoeng world - or a combination of both.

My concern is that things might be a bit more serious than that. If we consider 
a warmer world with the same level of precipitation, the surface evaporation 
world be higher and the relative atmospheric humidity would (I think) be lower. 
As a result, soil wetness may be very much lower, as  evapotranspiration would 
be higher. If rainfall patterns were perturbed, we might additionally get more 
variability in both wetness and precipitation.

So we could end up in a world with much drier soils, and possibly heavier 
storms, too.

Should your vectors therefore be soil wetness vs temperature, not precipitation 
vs temp?  Making a bad call on this could really hit agricultural outputs.

A
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