SOLAR GEOENGINEERING WEEKLY SUMMARY (15 APRIL - 21 APRIL 2024)
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By Andrew Lockley
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RESEARCH PAPERSA protocol for model intercomparison of impacts of Marine
Cloud Brightening Climate Intervention
<https://egusphere.copernicus.org/preprints/2024/egusphere-2024-1031/>

Rasch, P., Hirasawa, H., Wu, M., Doherty, S., Wood, R., Wang, H., ... &
Singh, H. (2024). A protocol for model intercomparison of impacts of Marine
Cloud Brightening Climate Intervention. *EGUsphere*, *2024*, 1-43.

*Abstract*

A modeling protocol is introduced (defined by a series of model simulations
with specified model output). The protocol is designed to improve
understanding of climate impacts from Marine Cloud Brightening (MCB)
Climate Intervention. The model simulations are not intended to assess
consequences from a realistic MCB deployment intended to achieve specific
climate targets but instead to expose responses produced by MCB
interventions in 6 regions with pervasive cloud systems that are often
considered as candidate regions for such a deployment. A calibration step
involving simulations with fixed sea surface temperatures is first used to
identify a common forcing, and then coupled simulations with forcing in
individual regions and combinations of regions are used to examine climate
impacts. Synthetic estimates constructed by superposing responses from
simulations with forcing in individual regions are considered as a means to
approximate the climate impacts produced when MCB interventions are
introduced in multiple regions.

A few results comparing simulations from 3 modern climate models (CESM2,
E3SMv2, UKESM1) are used to illustrate similarities and differences between
model behavior and the utility of estimates of MCB climate responses that
have been synthesized by summing responses introduced in individual
regions. There are substantial differences in the cloud responses to
aerosol injections between models, but the models often show strong
similarities in precipitation and surface temperature response signatures
when forcing is imposed with similar amplitudes in common regions.

Shedding light on the increased carbon uptake by a boreal forest under
diffuse solar radiation across multiple scales
<https://pubmed.ncbi.nlm.nih.gov/38624252/>

Neimane‐Šroma, S., Durand, M., Lintunen, A., Aalto, J., & Robson, T. M.
(2024). Shedding light on the increased carbon uptake by a boreal forest
under diffuse solar radiation across multiple scales. *Global Change
Biology*, *30*(4), e17275.

*Abstract*

Solar radiation is scattered by cloud cover, aerosols and other particles
in the atmosphere, all of which are affected by global changes.
Furthermore, the diffuse fraction of solar radiation is increased by more
frequent forest fires and likewise would be if climate interventions such
as stratospheric aerosol injection were adopted. Forest ecosystem studies
predict that an increase in diffuse radiation would result in higher
productivity, but ecophysiological data are required to identify the
processes responsible within the forest canopy. In our study, the response
of a boreal forest to direct, diffuse and heterogeneous solar radiation
conditions was examined during the daytime in the growing season to
determine how carbon uptake is affected by radiation conditions at
different scales. A 10-year data set of ecosystem, shoot and forest floor
vegetation carbon and water-flux data was examined. Ecosystem-level carbon
assimilation was higher under diffuse radiation conditions in comparison
with direct radiation conditions at equivalent total photosynthetically
active radiation (PAR). This was driven by both an increase in shoot and
forest floor vegetation photosynthetic rate. Most notably, ecosystem-scale
productivity was strongly related to the absolute amount of diffuse PAR,
since it integrates both changes in total PAR and diffuse fraction. This
finding provides a gateway to explore the processes by which absolute
diffuse PAR enhances productivity, and the long-term persistence of this
effect under scenarios of higher global diffuse radiation.

Speed of environmental change frames relative ecological risk in climate
change and climate intervention scenarios
<https://www.nature.com/articles/s41467-024-47656-z>

Hueholt, D. M., Barnes, E. A., Hurrell, J. W., & Morrison, A. L. (2024).
Speed of environmental change frames relative ecological risk in climate
change and climate intervention scenarios. *Nature Communications*, *15*(1),
3332.

*Abstract*

Stratospheric aerosol injection is a potential method of climate
intervention to reduce climate risk as decarbonization efforts continue.
However, possible ecosystem impacts from the strategic design of
hypothetical intervention scenarios are poorly understood. Two recent Earth
system model simulations depict policy-relevant stratospheric aerosol
injection scenarios with similar global temperature targets, but a 10-year
delay in intervention deployment. Here we show this delay leads to distinct
ecological risk profiles through climate speeds, which describe the rate of
movement of thermal conditions. On a planetary scale, climate speeds in the
simulation where the intervention maintains temperature are not
statistically distinguishable from preindustrial conditions. In contrast,
rapid temperature reduction following delayed deployment produces climate
speeds over land beyond either a preindustrial baseline or no-intervention
climate change with present policy. The area exposed to threshold climate
speeds places different scenarios in context to their relative ecological
risks. Our results support discussion of tradeoffs and timescales in future
scenario design and decision-making.

Regional Welfare Impacts from Options for Limiting Global Average
Temperature <https://www.researchsquare.com/article/rs-4009794/v1>

Ding, C., Kim, S., Singer, C., & Sriver, R. (2024). Regional Welfare
Impacts from Options for Limiting Global Average Temperature.

*Abstract*

Extrapolation of historical trends in anthropogenic atmospheric carbon
dioxide emissions is compared to results with new policy options. One
approach is to multiply historical extrapolation of global emissions by a
factor with a decline from 1 to a smaller multiple, e.g. on a timescale of
about 30 years. Another allows for solar radiation management via
anthropogenic stratospheric sulfur injection by one or more of sixteen
geographic regions, in order to limit global average temperature to a
chosen target level. An economic measure of impacts on human welfare is
compared for different versions of these two approaches. That measure is
time-integrated discounted utility of per capita consumption. That measure
is computed with and without empathy, which involves geographical regions
counting part of others’ welfare as part of their own. Inter-regional fund
transfers that cover all or part of a region’s expenditures used for
limiting carbon emissions can be used to encourage broader inter-regional
cooperation. These exercises pose interesting questions about how choices
will ultimately be made between use of one or both of carbon emissions
limitations and solar radiation management.

A fully coupled solid particle microphysics scheme for stratospheric
aerosol injections within the aerosol-chemistry-climate-model SOCOL-AERv2
<https://egusphere.copernicus.org/preprints/2024/egusphere-2024-444/>

Vattioni, S., Weber, R., Feinberg, A., Stenke, A., Dykema, J. A., Luo, B.,
... & Chiodo, G. (2024). A fully coupled solid particle microphysics scheme
for stratospheric aerosol injections within the
aerosol-chemistry-climate-model SOCOL-AERv2. *EGUsphere*, *2024*, 1-41.

*Abstract*

Recent studies have suggested that injection of solid particles such as
alumina and calcite particles for stratospheric aerosol injection (SAI)
instead of sulfur-based injections could reduce some of the adverse side
effects of SAI such as ozone depletion and stratospheric heating. Here, we
present a version of the global aerosol-chemistry-climate model SOCOL-AERv2
and the Earth System Model (ESM) SOCOLv4 which incorporate a solid particle
microphysics scheme for assessment of SAI of solid particles. Microphysical
interactions of the solid particle with the stratospheric sulfur cycle were
interactively coupled to the heterogeneous chemistry scheme and the
radiative transfer code (RTC) for the first time within an ESM. Therefore,
the model allows simulation of heterogeneous chemistry at the particle
surface as well as feedbacks between microphysics, chemistry, radiation and
climate. We show that sulfur-based SAI results in a doubling of the
stratospheric aerosol burden compared to the same injection rate of calcite
and alumina particles with radius of 240 nm, mainly due to the smaller
density and the smaller average particle size of sulfuric acid aerosols and
thus, slower sedimentation. Therefore, to achieve the same radiative
forcing, larger injection rates are needed for calcite and alumina particle
injection than for sulfur-based SAI. The stratospheric sulfur cycle would
be significantly perturbed, with a reduction in stratospheric sulfuric acid
burden by 53 %, when injecting 5 Mt/yr of alumina or calcite particles of
240 nm radius. We show that alumina particles will acquire a sulfuric acid
coating equivalent of about 10 nm thickness, if the sulfuric acid is
equally distributed over the whole available particle surface area in the
lower stratosphere. However, due to a steep contact angle of sulfuric acid
on alumina particles, the sulfuric acid coating would likely not cover the
entire alumina surface, which would result in available surface for
heterogeneous reactions other than the ones on sulfuric acid. When applying
realistic uptake coefficients of 1.0, 10-5 and 10-4 for H2SO4, HCl and
HNO3, respectively, the same scenario with injections of calcite particles
results in 94 % of the particle mass remaining in the form of CaCO3. This
likely keeps the optical properties of the calcite particles intact, but
could significantly alter the heterogeneous reactions occurring on the
particle surfaces. The major process uncertainties of solid particle SAI
are 1) the solid particle microphysics in the injection plume and degree of
agglomeration of solid particles on the sub-ESM grid scale, 2) the
scattering properties of the resulting agglomerates 3) heterogeneous
chemistry on the particle surface and 4) aerosol-cloud interactions. These
uncertainties can only be addressed with extensive, coordinated,
experimental and modelling research efforts. The model presented in this
work offers a useful tool for sensitivity studies and impact analysis of
new experimental results on points 1) to 3) for SAI of solid particles.

Possible Mitigation of Global Cooling due to Supervolcanic Eruption via
Intentional Release of Fluorinated Gases
<https://essopenarchive.org/users/540715/articles/642445-possible-mitigation-of-global-cooling-due-to-supervolcanic-eruption-via-intentional-release-of-fluorinated-gases>

Xu, Y., Ribar, N. P., Schade, G. W., Lockley, A. J., Zhang, Y. G., Sachnik,
J., ... & Velders, G. J. (2023). Possible Mitigation of Global Cooling due
to Supervolcanic Eruption via Intentional Release of Fluorinated
Gases. *Authorea
Preprints*.

*Abstract*

Supervolcanic eruptions induced abrupt global cooling (roughly at a rate of
~1ºC/year lasting for years to decades), such as the prehistoric
Yellowstone eruption released, by some estimates, SO2 about 100 times
higher than the 1991 Mt. Pinatubo eruption. An abrupt global cooling of
several ºC, even if only lasting a few years, would present immediate and
drastic stress on biodiversity and food production - posing a global
catastrophic risk to human society. Using a simple climate model, this
paper discusses the possibility of counteracting supervolcanic cooling with
the intentional release of greenhouse gases. Although well-known
longer-lived compounds such as CO2 and CH₄ are found to be unsuitable for
this purpose, select fluorinated gases (F-gases), either individually or in
combinations, may be released at gigaton scale to offset most of the
supervolcanic cooling. We identify candidate F-gases (viz. C4F6 and CH3F)
and derive radiative and chemical properties of ‘ideal’ compounds matching
specific cooling events. Geophysical constraints on manufacturing and
stockpiling due to mineral availability are considered alongside technical
and economic implications based on present-day market assumptions. The
consequences of F-gas release in perturbing atmospheric chemistry are
discussed in the context of those due to the supervolcanic eruption itself.
The conceptual analysis here suggests the possibility of mitigating certain
global catastrophic risks via intentional intervention.

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WEB POSTSLet’s talk about geoengineering!
<https://www.linkedin.com/pulse/lets-talk-geoengineering-tamas-bodai-mynyf>
(LinkedIn)Why We Need To Share Knowledge With Young People On The Ground:
Lessons Learned From Nairobi And Mombasa
<https://sgdeliberation.org/why-we-need-to-share-knowledge-with-young-people-on-the-ground-lessons-learned-from-nairobi-and-mombasa/>
(DSG)Startups want to geoengineer a cooler planet. With few rules, experts
see big risks
<https://www.npr.org/2024/04/21/1244357506/earth-day-solar-geoengineering-climate-make-sunsets-stardust>
(NPR)
<https://www.npr.org/2024/04/21/1244357506/earth-day-solar-geoengineering-climate-make-sunsets-stardust>
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*UPCOMING EVENTS**(NEW) Dr Alan Gadian on Marine Cloud Brightening by HPAC
<https://groups.google.com/g/geoengineering/c/h0FQLRf9T3g> | 29 April
2024**Fourteenth
GeoMIP Workshop | Ithaca, USA
<https://climate.envsci.rutgers.edu/GeoMIP/2024.html> | 10-12 July 2024*

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------------------------------
PODCASTSAI and international conflict - Morrissey | Reviewer 2 does
geoengineering

SAI and international conflict - Morrissey

Reviewer 2 does geoengineering

1:24:52
<https://podcasts.apple.com/us/podcast/sai-and-international-conflict-morrissey/id1529459393?i=1000652616830&uo=4>

"William Morrissey explains how SAI could lead to conflict and
counter-geoengineering. @geoengineering1 isn't convinced it will all end so
badly.

Avoiding atmospheric anarchy: Geoengineering as a source of interstate
tension —William Morrissey

https://doi.org/10.1177/27538796231221597";

------------------------------
YOUTUBE VIDEOPlaying God? Weather Change Experiments in San Francisco | CBN
News <https://www.youtube.com/watch?v=0vR2xcdu5Ac>

"What are the consequences of this? Potentially catastrophic." Scientists
onboard a decommissioned aircraft carrier are conducting marine cloud
brightening experiments hoping to stop global warming. The CO2 Coalition's
Greg Wrightstone says first, the scientists must consider the Hippocratic
oath to "do no harm."

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