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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