Dear Colleagues,

1) At a recent 3/6/2023 NOAC meeting there was an extra ordinarily lively
and fruitful discussion on this topic that featured representatives of a
very broad spectrum of views that (as one participant remarked) was unusual
in that it was a respectful discussion and airing of view points rather
than a debate.  Unfortunately, I was unable to attend this meeting but was
able to view the recording of it, and strongly encourage all who are able
to, to access this recording to view it.  As recordings of NOAC meetings
are not generally distributed more broadly than the NOAC list I don’t feel
at liberty to include a link to this recording in this post to other lists.
For this reason, and also because I will likely misinterpret or not do
justice to them, I will refrain from attaching (my understanding of)
viewpoints discussed to particular persons at the meeting.

2) The letters supporting SRM research (letter #1
<https://climate-intervention-research-letter.org/> and letter # 2
<https://www.call-for-balance.com/letter> are commendable developments that
should be welcome by all direct climate cooling (DCC) advocates. However
(as noted by some in the NOAC meeting) they are:

 a) Cautious to a fault on quick or gradual piloting and deployment
(depending on method see below), given the urgency of triggering irreversible
tipping points
<https://www.google.com/search?client=firefox-b-1-d&q=lenton+NAS+workshop+on+tipping+points2022#fpstate=ive&vld=cid:2d77e4e5,vid:4ppkTB4_fyk>
potential to prevent or reduce increased catastrophic harm to humans and
the fact that (mentioned by some participants) that the Mt. Pinatubo volcano
<https://earthobservatory.nasa.gov/images/1510/global-effects-of-mount-pinatubo>
for example lofted about 17 million tons of SO2 to the stratosphere (far
more at one time than any SAI planned deployment that I am aware of) and
cooled the globe by roughly 0.6 C for 15 months without any (at least
prominently publicized) adverse impacts.

b) Too narrowly focused on SRM and particularly (global) SAI to the
exclusion of other generally lower-leverage and lower-risk possible direct
climate cooling methods
<https://pdfhost.io/v/kUvEpsGdb_Understanding_the_Urgent_Need_for_Direct_Climate_Cooling_0209233>
(DCC), in spite of emphasizing (in the spirit of “not placing one’s eggs
all in one basket”) the need to study MCB and CCN as well as SAI as
“outcomes might be optimized if multiple techniques are used in
combination” (Letter 1).  Letter 2 is less specifically directed at these
three species of SRM but still exclusively focused on SRM and from the
points made on p. 7 for example that “the provision of SRM is organized by
a globally legitimized body, and not based on private interests” on
high-leverage SRM with global scope. For example, as recent modeling
suggests that if and when we achieve (human and natural) net-zero GHG
emissions global temperature will not significantly drop
<https://www.carbonbrief.org/explainer-will-global-warming-stop-as-soon-as-net-zero-emissions-are-reached/>
for at least another 50 years due to legacy heat from the Ocean (where 90%
of it is being stored), and even more recent modeling suggests that 7-10 C
may be “in the pipeline
<https://arxiv.org/ftp/arxiv/papers/2212/2212.04474.pdf>” (most of which is
undoubtedly related to ocean warming where 90% of legacy warming is being
stored) even if net-zero were achieved today, it would seem that we should
urgently begin researching and when prudent implementing methods to reduce
(and possible use for economic benefit) this excess ocean “heating from
below” in addition to doing the same for “heating from above (see OTEC
summary here
<https://docs.google.com/document/d/1TowThwi6j6cX3iLGBRrj22D30cYhKa_9/edit>
).  Another example is cooling based on efforts to enhance water cycle
cooling through evapotranspiration and convection that may also regenerate
nature (just as important as reducing GHG’s in the long run
<https://www.cpegonline.org/post/our-two-climate-crises-challenge>) and
provide economic benefits (see for example Seatomizers summary here
<https://pdfhost.io/v/kUvEpsGdb_Understanding_the_Urgent_Need_for_Direct_Climate_Cooling_0209233>).


c) Assume an overly binary view of (and direct climate cooling) “global SAI
deployment or not” (my guess is with a now outdated (per research in b)
view of SAI “shaving the peak” (Shepherd and Long napkin diagram
<http://jgshepherd.com/wp-content/uploads/2011/01/Napkin-diagram.pdf>)
deployment that may be necessary in the future),  and  “research and
deployment” of direct climate cooling in general.  Regarding the first
binary there is no reason why any of the less risky direct climate cooling
methods discussed in b) should not (if found to be indeed effective and
with little risk) deployed asap, and (as mentioned by at least one
participant per the  “Cornell SAI group”) the most prudent roll-out of SAI
not be based on “nailing down the research” and then deploying, but rather
researching as much as possible while gradually deploying and evaluating
and researching further depending on outcomes in the spring  in polar
regions where the stratosphere is lower so that lofting with more
conventional aircraft may be possible , and the aerosol is likely to drop
out of the Stratosphere more quickly in months rather than years reducing
“termination shock” risk (see SAI summary here
<https://pdfhost.io/v/kUvEpsGdb_Understanding_the_Urgent_Need_for_Direct_Climate_Cooling_0209233>).
 And with regard to the “research and deployment” binary, assume (as one
NOAC meeting participant opined) that controlled experiments in
laboratories are inherently more valuable than field experiments as causal
factors can be elevated to extreme levels to facilitate signal (or outcome)
detection. But it seems to me that, as many have opined, atmospheric
processes and chemistry are so complex that we will never be certain that
we have adequately pinned it down with laboratory or small-scale empirical
research.  One participant asked a key question in this regard. At what
empirical scope do we need to research to be confident that risk is low
enough to start deploying. It seems to be rather self-evident that the best
and only way to reach this point would be to proceed with very small
localized deployments in the poles and constantly monitor, adjust, and
learn by doing, that is that a good part of the “research” is the
“gradually deployment”.  After all we’re not addressing nuclear radiation
or the Manhattan project here, we’re primarily talking about a natural
substance millions of tons of which have (and will be continued in the
future) to be lofted into the atmosphere by natural methods!  In this sense
I would suggest that empirical research on, particularly atmospheric and
cloud-based DCC, will likely require more “social science” non-controlled
experiment statistical techniques in the “real atmosphere” that can only be
accomplished with small-scale deployment.

d) And as one NOAC meeting participant noted, Letter 1 includes a rather
gratuitous (in the offering any evidence in support) swipe at the Make
Sunsets effort particularly with regard to selling “cooling credits that I
too think is unwarranted and counterproductive (see discussion of Make
Sunsets initiative in 3) below):  *“The state of scientific knowledge about
SRM is also currently insufficient for it to be included as part of a
climate credit system or other commercial offering, as some have started to
propose.* Even for stratospheric aerosol injection (the most
well-understood SRM approach), the amount of cooling achieved by the
injection of a given mass of material and how SAI will affect the climate
system are still highly uncertain. Even with improved understanding of
these effects, since SRM does not address the cause of climate change, nor
all of the effects of increased greenhouse gas concentrations, it likely
will never be an appropriate candidate for an open market system of credits
and independent actors.”

3) Finally, I believe that this entire topic of “how can best move the ball
forward on urgently necessary DCC” should be considered in a broad
political as well as scientific frame.

a) If I may say so, as a social scientist, and especially as a radical
economist, I believe that I am particularly a-tuned to the political
dimensions of social change and “social ideology” as mainstream economics
is a prime example of the latter (I wrote a book on this that I will send
to anyone upon request). Similarly, I think the broad NOAC discussion that
included members of our broader “climate cooling community” including but
not exclusively climate scientists or climate change professionals who
(consciously or not) understandably may have to be more careful and
conservative in their public positions on these issues. All of us (people
and organizations) are (again not always consciously) playing a strategic
role in this sense.

b) My own view (that comes without personal cost to my livelihood, status,
and/or strategic and practical efforts to make the world a better place) is
that anything that stimulates awareness, debate, and hopefully action on
the need for urgent direct climate cooling, and that is physically or
economically beneficial, or at the very least, does not cause harm, is a
positive step forward. For example, I believe that all of us (including the
founders of Make Sunsets) understand that an effective high-leverage (and
therefore high-risk) direct climate cooling method like SAI should be
researched and implemented publicly and transparently, or with extensive
public monitoring and oversight, per the two recent letters on this topic
discussed in 2) above. And since the Make Sunsets’ lofting of “de-minimis”
amounts of SO2 to the stratosphere is not “effective” in terms of climate
cooling <https://makesunsets.com/blogs/news/pricing-cooling-credits>, and
thus does not cause any harm and has the same temporary cooling affect as a
much large amount of GHG reduction  would permanently (see below) it is on
balance a positive step toward cooling.

c) I believe that the Make Sunsets selling of DDC credits that can be
roughly estimated in this case, as generally speaking (see below) global
SAI cooling can be viewed (like GHG removal) as a pure “public good” that
has the same result no matter where and when it is applied, has enhanced
it’s political impact and has the potential to create a broad group of
citizen/consumer climate cooling advocates among the general public.
Hopefully, this will facilitate kick start this possibility for other
(likely more local and geographically priced) legitimate private cooling
credits.  As I’ve said in prior blogs, I believe that we are in an “all
hands on deck” for cooling moment, and therefore need to harness whatever
institutional (public, non-profit, private) methods we can to ramp this up
as fast and as much as possible.

d) Finally, though what Make Sunsets is currently doing is not “effective”
in terms of climate, it is (modestly) physically beneficial as each gram of
SO2 actually lofted to the stratosphere is roughly equivalent to the
removal of 0.476 metric tons of CO2 for 2.1 years (see blog
<https://makesunsets.com/blogs/news/calculating-cooling>) as 1/2.1= 0.476),
so that (as pointed by Make Sunsets in the NOAC discussion) lofting a
kilogram of SO2 would be roughly equivalent to removing 476 metric tons of
CO2 for 2.1 years. And this linking of temporary cooling to temporary GHG
drawdown adds another useful “direct climate cooling” public education
dimension to the Make Sunsets effort as it shows how much temporary cooling
“bang for the buck” lofting a still “de-minimis” amount of SO2 can provide
relative to temporary removal of GHG.

e) Similarly, I believe that Andrew Lockley’s balloon lofting experiment,
though unfortunately named, can be viewed as a politically positive DCC
intervention.

As I said, that NOAC meeting stimulated a lot of good discussion!

Best,

Ron
,

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