Accepted for publication in Nature Climate Change (perspectives piece), but I 
note that the version Andrew attached wasn’t the final version (lots of good 
reviewer feedback).  Apologies that I can’t find the final version on my 
laptop, so you might have to wait for NCC to format it for the final version – 
hopefully soon.

 

There’s an obvious but often overlooked fundamental message here that the 
evaluation of SRM depends strongly on the scenario assumed… the number of times 
we all see statements that “solar geoengineering will do X” when there’s a 
buried assumption about the deployment strategy is remarkable, and we think we 
need to get beyond that; solar geoengineering is not a binary choice where 
either we do or don’t use it, but it seems like most of the discourse 
implicitly assumes that it is. 

 

doug

 

From: [email protected] [mailto:[email protected]] 
On Behalf Of Robert Chris
Sent: Thursday, January 15, 2015 1:32 AM
To: [email protected]
Subject: [geo] Re: A temporary, moderate, and responsive scenario for solar 
geoengineering, Keith and MacMartin

 

This paper is dated Feb 2014.  Is it peer reviewed?  Was it published and if so 
where?  A quick Google Scholar search throws up nothing.

Robert Chris

On Saturday, 10 January 2015 00:23:21 UTC, andrewjlockley wrote:

(Attached) 

A temporary, moderate, and responsive scenario for solar geoengineering   

David W. Keith and Douglas G. MacMartin

Abstract 

Evaluation of the risks and benefits of solar geoengineering, or Solar 
Radiation Management (SRM) depend on the scenario for its implementation. 
Claims that SRM will reduce precipitation, increase ocean acidification, 
deplete stratospheric ozone, or that it must be continued forever once started 
are not inherent features of SRM but rather depend on the specific technology 
and time trajectory for implementation. We argue that the common assumption 
that SRM would be used to restore temperatures to preindustrial is a poor 
scenario choice on which to base policy-relevant judgments about the utility of 
SRM. As a basis for further analysis we provide a scenario that is temporary in 
that its end point is zero SRM, is moderate in that it offsets only half of the 
growth in other anthropogenic climate forcing, and is responsive in that it 
explicitly recognizes that the amount of SRM will be adjusted in light of new 
information. We provide specific quantitative illustrations of such a scenario 
for the case of stratospheric sulfate aerosols.  

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