Thanks for the useful feedback and responses to this question everyone. Its
not an area I have expertise in, so the feedback has been exceptionally
useful,
Kind Regards
Gideon

On Thu, 28 Jul 2022 at 15:09, Douglas MacMartin <dgm...@cornell.edu> wrote:

> I agree that the sign of the effect is unclear in addition to the
> magnitude, that is, nuclear winter + termination is “better” at first than
> nuclear winter alone, but “worse” afterwards if it is impossible to
> restart; that of course is all contingent on how bad the nuclear winter is,
> how much cooling is being offset, and your beliefs about how the use of SRM
> does or doesn’t affect mitigation (that is, the circumstances in which
> termination materially affects outcomes are those in which SRM is being
> used to offset significant warming – so from a risk perspective, if the
> counterfactual is that much warmer world, or the counterfactual a world
> that had more mitigation, is essential).
>
>
>
> I agree that as researchers we should try to inform decisions, and hence
> risks, and be responsive to stakeholder concerns.  In this case, I think
> the **much** bigger influence of SRM on nuclear winter comes from whether
> it increases or decreases the risks of nuclear war, and what we can do in
> terms of governance to affect that…
>
>
>
> *From:* Gideon Futerman <ggfuter...@gmail.com>
> *Sent:* Wednesday, July 27, 2022 6:10 PM
> *To:* Douglas MacMartin <dgm...@cornell.edu>
> *Cc:* gdebrou...@gmail.com; Daniele Visioni <daniele.visi...@gmail.com>;
> geoengineering <geoengineering@googlegroups.com>
> *Subject:* Re: [geo] Nuclear Winter and SRM (including termination shock)
>
>
>
> I think this is going to get into more general philosophy/ethics around
> Existential Risks, Longtermism and Global Catastrophic Risks, which whilst
> interesting and useful, probably a bit orthogonal to what people are
> turning to the geoengineering google group for. But basically, a difference
> between 6 billion and say 6.1 billion or 6.5 billion is firstly important
> from the perspective of deaths: that's still 100 million people. Secondly,
> climatic effects, excess deaths on top of the nuclear winter (or reduced
> severity!)  etc are potentially relevant for whether it will "only" kill 6
> billion and whether it will lead to irrecoverable (not merely awful)
> societal collapse, which from various longtermist perspectives is very bad.
> Given how hard it would be to recover anyway, a "double catastrophe" could
> make recovery much harder distinguish between a  Global Catastrophic Risk
> and an existential risk, which from various philosophical viewpoints is
> very important.
>
> Thus, such a question ie whether SRM might increase/decrease the
> likelihood of a global catastrophic risk being converted to an existential
> risk (due to this Latent Risk of termination shock we have been discussing)
> is of serious interest to many people, including potentially major funders
> who are potentially interested in investing in SRM research. In that sense,
> this impacts some potentially very important decisions for the future of
> our field, and the distinction between 6 billion and say 6.5 billion, or
> even if it just makes societal recovery 10% less likely to happen, it may
> be absolutely vital. I am happy to explain this in more depth if people
> need, although what I was really wanting to ask the list for was
> fundamentally a question of physical science to try and answer this
> application.
>
> Even if none of this has convinced you of the moral importance of it, the
> question I was asking was fundamentally a physical one, responding to a
> scientific assumption in Baum et al 2013 that I thought seemed potentially
> unsound (that under nuclear war termination shock would lead to a double
> catastrophe and not a slight softening of the first catastrophe). Given
> that paper is one of only a handful papers published in this intersection
> between SRM and Global Catastrophic Risk studies, such a claim is, even
> from a physical/empirical rather than moral viewpoint, important to test.
> Hence why I have posed this question.
>
>
>
>
>
> On Wed, 27 Jul 2022 at 19:59, Douglas MacMartin <dgm...@cornell.edu>
> wrote:
>
> All of the above, with qualifiers… yes the climatic response would be
> different, but personally I think 6B dead is so bad that whether it’s 6.01
> or 6.1 or 6.5 isn’t something that I feel matters particularly (nor do I
> think it is particularly answerable).  What decisions would depend on the
> answer to that question?
>
>
>
> *From:* Gideon Futerman <ggfuter...@gmail.com>
> *Sent:* Wednesday, July 27, 2022 1:31 PM
> *To:* Douglas MacMartin <dgm...@cornell.edu>
> *Cc:* gdebrou...@gmail.com; Daniele Visioni <daniele.visi...@gmail.com>;
> geoengineering <geoengineering@googlegroups.com>
> *Subject:* Re: [geo] Nuclear Winter and SRM (including termination shock)
>
>
>
> Hi Doug,
>
> Apologies for misinterpreting. Its a statement like this that I have been
> looking for.
>
> When you suggest it isn't appreciably worse, is that a suggestion that
> either:
>
> - The death toll/ the ability for society to recover would be no different
> given the double catastrophe than the single catastrophe
>
> - The climatic response to the double catastrophe is no different than the
> single catastrophe
>
> - The difference in death toll may be, say (and these are made up numbers)
> 6 billion vs 6.01 billion
>
> Thank you so much for the clarification
>
> Best
>
> Gideon
>
>
>
> On Wed, 27 Jul 2022 at 17:58, Douglas MacMartin <dgm...@cornell.edu>
> wrote:
>
> Of course there are more minor conflicts possible with less severe
> outcomes… though if it’s a regional war that doesn’t itself end
> civilization, I don’t see why one couldn’t restart SRM in a year or two if
> desired.
>
>
>
> Gideon, you write: “I understand why there is aversion to me exploring
> such risks;” I think you misunderstand everyone’s response here.  It
> isn’t an aversion to exploring them, nor a belief that we don’t need to
> look at extreme but less likely scenarios, but rather, that this specific
> risk doesn’t seem to many of us like there’s anything that needs to be
> explored.  That is, my view, and I think others, is that any nuclear war
> severe enough to result in losing the ability to even restart SRM is so
> severe that the nuclear war + termination isn’t appreciably worse than the
> nuclear war itself.
>
>
>
> I 100% agree with the need to think through low probability but high
> impact possibilities.
>
>
>
> d
>
>
>
> *From:* geoengineering@googlegroups.com <geoengineering@googlegroups.com> *On
> Behalf Of *Gilles de Brouwer
> *Sent:* Tuesday, July 26, 2022 11:11 PM
> *To:* ggfuter...@gmail.com
> *Cc:* Daniele Visioni <daniele.visi...@gmail.com>; geoengineering <
> geoengineering@googlegroups.com>
> *Subject:* Re: [geo] Nuclear Winter and SRM (including termination shock)
>
>
>
> 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 <ggfuter...@gmail.com>
> 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, <daniele.visi...@gmail.com>
> 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 <ggfuter...@gmail.com> 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:
> rob...@envsci.rutgers.edu
> 14 College Farm Road            http://people.envsci.rutgers.edu/robock
> New Brunswick, NJ 08901-8551     ☮ https://twitter.com/AlanRobock
>
> 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:
> rob...@envsci.rutgers.edu
> 14 College Farm Road            http://people.envsci.rutgers.edu/robock
> New Brunswick, NJ 08901-8551     ☮ https://twitter.com/AlanRobock
>
> 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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