FYI   Updated nuclear winter analysis is so much worse than SAI that it's
pointless to consider.

*Nuclear winter revisited with a modern climate model and current nuclear
arsenals: Still catastrophic consequences*
Alan Robock,1 Luke Oman,1,2 and Georgiy L. Stenchikov1
Received 8 November 2006; revised 2 April 2007; accepted 27 April 2007;
published 6 July 2007
https://climate.envsci.rutgers.edu/pdf/RobockNW2006JD008235.pdf

Gilles de Brouwer


On Tue, Jul 26, 2022 at 5:50 PM Gideon Futerman <[email protected]>
wrote:

> Apologies, you are correct, I was using the ECS values from AR5 and forgot
> it had reduced with AR6. I was also getting my range vs values mixed up.
> Nonetheless, a similar point still broadly stands- the ipcc suggests with
> only medium confidence that it is "very likely" that ECS is between 2K and
> 5K (not 6K as I had previously stated), putting a warming of anything above
> 5K therefore at between 0-5% probability with medium confidence.
> Whilst I appreciate the desire to focus on the median ECS, I think it is
> nonetheless important to consider the more extreme, fat tailed risks. Not
> because these will happen or are likely to happen, but because in general
> such worse case scenario, low probability high impact scenarios are
> neglected.
> This is the same reason I care about SRM in concert with a nuclear war.
> Not because I want to overplay how important SRM is under such a scenario,
> but merely want to explore the worse case scenarios. I don’t think
> (certainly hope not) that any of the scenarios the RESILIENCER Project
> explores are likely, certainly none are the median scenarios. Rather, they
> are those scenarios in the fat tails of the possible risks.
> I understand why there is aversion to me exploring such risks; I would
> hate people to think that I am claiming the research community at large
> should start focusing on such risks (which would be foolish). Nonetheless,
> it seems odd to not at least some degree look at these more extreme, much
> less likely, scenarios.
>
> On Tue, 26 Jul 2022, 22:33 Daniele Visioni, <[email protected]>
> wrote:
>
>> Dear Gideon,
>> not to pile on but I feel like this should be corrected: none of the most
>> current IPCC projections say that 550ppm have a 10% chance of leaving us
>> with 6K of warming.
>> Even the most high sensitivity models in CMIP6 only show a ECS of, at
>> most, 5 per doubling of CO₂ (so 560), but the best estimate is still around
>> 3K given a whole range of approaches to estimate it.
>> For more relevant IPCC scenarios during this century, given transient
>> sensitivity and more, scenarios that lead to 550ppm (considering also other
>> GHG, LUC, aerosols) like SSP2-4.5 have a median warming of a bit less than
>> 3K.
>> How can surely say the IPCC is wrong and climate models are wrong, of
>> course.
>>
>> (Ça vas sans dire, I’m not trying to downplay climate change! But being
>> precise helps having better discussions :) )
>>
>>
>> On 26 Jul 2022, at 17:20, Gideon Futerman <[email protected]> wrote:
>>
>> Dear Dr Robock,
>> Whilst I would admit that 3K of cooling by SRM is unlikely, it is
>> certainly not out of the range of possibility. Given CO2 concentrations of
>> 550PPM have a 10% chance of leaving us with 6K of warming (and that
>> certainly doesn't seem to be an unreasonable amount of emissions given
>> mitigation trajectories), it certainly doesn't seem like there is a less
>> than 10% probability of a given deployment scheme being 3K of forcing.
>> Secondly, why care about this if there is a nuclear war. Maybe you are
>> correct, and there is no worry. But if you care about post-nuclear war
>> societal recovery, it may be important to know whether SRM-driven
>> termination shock makes that more or less likely, or is entirely
>> negligible. Of course, the primary worry here is avoid the initial
>> catastrophe (nuclear war). Nonetheless, the question of whether SRM
>> termination shock under nuclear war has any effect (even if only 10% of the
>> magnitude of the effects of the nuclear war) is significant.
>> I am trying to look at low probability, heavy tailed risks of SRM,
>> including how it interacts with other risks. This is why I want to look at
>> the (relatively unlikely) scenario which I have laid out.
>> And apologies for the spelling mistake, spelling is certainly not my
>> strong suit!
>> Kind Regards
>> Gideon Futerman
>> He/Him
>> www.resiliencer.org
>> On Tuesday, 26 July 2022 at 16:05:48 UTC+1 Alan Robock wrote:
>>
>>> Dear Gideon,
>>>
>>> It is spelled "negligible."  And nobody is suggesting enough SAI to
>>> produce 3K cooling, because that means there has been no mitigation.
>>>
>>> A nuclear war could kill billions of people from starvation, and would
>>> collapse civilization, surely reducing greenhouse gas emissions.  Why would
>>> you even worry about global warming and geoengineering then?  That's why I
>>> say your are comparing two things that are of completely different scales.
>>>
>>>
>>> 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 10:59 AM, Gideon Futerman wrote:
>>>
>>> Dear Alan Robock,
>>> When you say overwhelm, is the suggestion here that the increase in
>>> radiative forcing from the termination of aerosol injection would be
>>> entirely negligable compared to the nuclear winter scenario?
>>> If SAI were masking 3K of warming, and you got a nuclear winter driven
>>> cooling of say 7K, surely the impact of the termination of SAI would not be
>>> negligable, even if it would be significantly less than the cooling of
>>> nuclear winter (ie you still get a nuclear winter)? I am trying to work out
>>> if the "double catastrophe" as Baum calls it actually applies in the
>>> nuclear winter scenario. So the question of whether the removal of the
>>> contribution of SAI to radiative forcing (by termination) makes the nuclear
>>> winter (and the resulting warming afterwards) worse, less bad or is
>>> entirely negligable is important.
>>> Moreover might sunlight removal effects be important in the short term,
>>> particularly if it were a relatively high SAI radiative forcing and
>>> (relatively) minor nuclear winter (say about 6K of cooling)? Given up to
>>> 50% of sulfate aerosols remain in the stratosphere up to 8 months after
>>> termination, would the added impact of the sulfate aerosols on top of the
>>> significantly more soot aerosols have an effect of sunlight available for
>>> photosynthesis, so increase impact on food production in the early days of
>>> the nuclear winter? Or would this simply be negligable in the face of the
>>> radiation reduction from even a relatively minor nuclear winter?
>>> Kind Regards
>>> Gideon
>>>
>>>
>>> On Tuesday, 26 July 2022 at 15:20:44 UTC+1 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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>>>>
>>>>
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