I'm  surprised Alan should neglect to cite studies other than his own, as 
 climate responses to carbon aerosols in the atmosphere vary greatly. The 
recent literature is illustrative- a growing  concern is the impact of 
black carbon from satellite and spacecraft launches, which may warm the 
upper atmosphere rather than cool it:

Journal of Geophysical Research: Atmospheres 
<https://agupubs.onlinelibrary.wiley.com/journal/21698996>  1June2022

The Climate and Ozone Impacts of Black Carbon Emissions From Global Rocket 
Launches
Christopher M Maloney 
<https://agupubs.onlinelibrary.wiley.com/action/doSearch?ContribAuthorRaw=Maloney%2C+Christopher+M>
, Robert W Portmann 
<https://agupubs.onlinelibrary.wiley.com/action/doSearch?ContribAuthorRaw=Portmann%2C+Robert+W>
, Martin N Ross 
<https://agupubs.onlinelibrary.wiley.com/action/doSearch?ContribAuthorRaw=Ross%2C+Martin+N>
, Karen H Rosenlof 
<https://agupubs.onlinelibrary.wiley.com/action/doSearch?ContribAuthorRaw=Rosenlof%2C+Karen+H>
 
https://doi.org/10.1029/2021JD036373

Aerosol emissions from spaceflight activities play a small but increasing 
role in the background stratospheric aerosol population. Rockets used by 
the global launch industry emit black carbon (BC) particles directly into 
the stratosphere where they accumulate, absorb solar radiation, and warm 
the surrounding air. We model the chemical and dynamical response of the 
atmosphere to northern mid-latitude rocket BC emissions. We initially 
examine emissions at a rate of 10 Gg per year, which is an order of 
magnitude larger than current emissions, but consistent with extrapolations 
of space traffic growth several decades into the future. We also perform 
runs at 30 and 100 Gg per year in order to better delineate the 
atmosphere's response to rocket BC emissions. We show that a 10 Gg/yr 
rocket BC emission increases stratospheric temperatures by as much as 1.5 K 
in the stratosphere. Changes in global circulation also occur. For example, 
the annual subtropical jet wind speeds slow down by as much as 5 m/s, while 
a 10%–20% weakening of the overturning circulation occurs in the northern 
hemisphere during multiple seasons. Warming temperatures lead to a ozone 
reduction in the northern hemisphere by as much as 16 DU in some months. 
The climate response increases in a near linear fashion when looking at 
larger 30 and 100 Gg emission scenarios. Comparing the amplitude of the 
atmospheric response using different emission rates provides insight into 
stratospheric adjustment and feedback mechanisms. Our results show that the 
stratosphere is sensitive to relatively modest BC injections.

On Tuesday, July 26, 2022 at 10:20:44 AM UTC-4 Alan Robock wrote:

> Dear Gideon,
>
> A nuclear war would be orders of magnitude worse than any impacts of SAI 
> or termination.  Soot from fires ignited by nuclear attacks on cities and 
> industrial areas would last for many years, and would overwhelm any impacts 
> from shorter lived sulfate aerosols.  Of course the impacts depend on how 
> much soot, but a war between the US and Russia could produce a nuclear 
> winter.  For more  information on our work and the consequences of nuclear 
> war, please visit http://climate.envsci.rutgers.edu/nuclear/
>
> Alan Robock
>
> Alan Robock, Distinguished Professor
> Department of Environmental Sciences         Phone: +1-848-932-5751 
> <(848)%20932-5751>
> Rutgers University                            E-mail: 
> [email protected]
> 14 College Farm Road            http://people.envsci.rutgers.edu/robock
> New Brunswick, NJ 08901-8551     ☮ https://twitter.com/AlanRobock
>
> [image: Signature] 
>
>
> On 7/26/2022 10:03 AM, Gideon Futerman wrote:
>
> As part of the RESILIENCER Project, we are looking at low probability high 
> impact events and their relation to SRM. One important worry in this 
> regards becomes termination shock, most importantly what Baum (2013) calls 
> a "Double Catastrophe" where a global societal collapse caused by one 
> catastrophe then causes termination shock, another catastrophe, which may 
> convert the civilisational collapse into a risk of extinction. 
>
> One such initial catastrophe may be nuclear war. Thus, the combination of 
> SRM and nuclear war may be a significant worry. As such, I am posing the 
> question to the google group: what would happen if SRM (either 
> stratospheric or tropospheric- or space based if you want to go there) was 
> terminated due to a nuclear war? What sort of effects would you expect to 
> see? Would the combination worsen the effects of nuclear war or help 
> ameliorate them? How would this differ between SRM types?
>
>
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