*SOLAR GEOENGINEERING WEEKLY SUMMARY (10 JUNE - 16 JUNE 2024*

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DEADLINES(NEW) Call for Abstract—Cloud and precipitation responses to
aerosol pollution, weather modification and climate intervention
<https://annual.ametsoc.org/index.cfm/2025/> | Deadline to apply: 15 August
2024
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RESEARCH PAPERSHow Does the Latitude of Stratospheric Aerosol Injection
Affect the Climate in UKESM1?
<https://egusphere.copernicus.org/preprints/2024/egusphere-2024-1565/>

Henry, M., Bednarz, E. M., & Haywood, J. (2024). How Does the Latitude of
Stratospheric Aerosol Injection Affect the Climate in UKESM1?. *EGUsphere*,
*2024*, 1-23.

*Abstract*

Stratospheric Aerosol Injection (SAI) refers to a climate intervention
method by which aerosols are intentionally added to the lower stratosphere
to enhance sunlight reflection and offset some of the adverse effects of
global warming. The climate outcomes of SAI depend on the location, amount,
and timing of injection, as well as the material used. Here, we isolate the
role of the latitude of SO2 injection by comparing different scenarios
which have the same global-mean temperature target, altitude of injection,
and hemispherically symmetric injection rates. These are: injection at the
equator (EQ), and injection at 15° N and S (15N+15S), at 30° N and S
(30N+30S), and at 60° N and S (60N+60S). We show that injection at the
equator leads to many undesirable side effects, such as a residual Arctic
warming, significant reduction in tropical precipitation, reductions in
high-latitude ozone, tropical lower stratospheric heating, and
strengthening of the stratospheric jets in both hemispheres. Additionally,
we find that the most efficient injection locations are the subtropics (15
and 30° N and S), although the 60N+60S strategy only requires around 30 %
more SO2 injection for the same amount of cooling; the latter also leads to
much less stratospheric warming but only marginally increases high-latitude
surface cooling. Finally, while all the SAI strategies come with
trade-offs, we demonstrate that the 30N+30S strategy has, on balance, the
least negative side effects and is easier to implement than a
multi-latitude controller algorithm; thus it is a good candidate strategy
for an inter-model comparison.

The Wizards of Climate Change: How Can Technology Serve Hope and Justice?
An Ethical Framework for Climate Intervention Research: What It Is and Why
You Should Care <https://www.zygonjournal.org/article/id/15389/>

Williams, B. M., Shimamoto, M. & Graumlich, L. J., (2024) “An Ethical
Framework for Climate Intervention Research: What It Is and Why You Should
Care”, Zygon: Journal of Religion and Science 59(1), 82–96.

*Abstract*

Climate change poses significant threats to ecosystems, human health, and
global stability. Despite international efforts to reduce greenhouse gas
emissions, the Earth’s climate continues to warm, leading to extreme
weather events, rising sea levels, and other detrimental impacts. In
response to this crisis, scientists have begun exploring various strategies
to mitigate climate change through geoengineering, which involves
deliberate interventions in the Earth’s climate system. This article
provides an overview of climate geoengineering research, focusing on key
techniques, challenges, and ethical considerations, including actions being
taken by the American Geophysical Union (AGU), a nonprofit professional
scientific society, to develop an ethical framework to help guide research
in this important area. AGU also is driving global engagement on this
topic, including with leaders and members of faith communities.

Changes in Shipping Emissions As a Natural Analogue for Climate
Intervention: Detecting and Attributing Changes Due to Specific Human
Activities As a Testbed for Future Controversies
<https://ams.confex.com/ams/104ANNUAL/meetingapp.cgi/Paper/431888?s=08>

Visioni, D., & Quaglia, I. (2024, January). Changes in shipping emissions
as a natural analogue for Climate Intervention: detecting and attributing
changes due to specific human activities as a testbed for future
controversies. In *104th AMS Annual Meeting*. AMS.

*Abstract*

In 2020, new regulations from the International Maritime Organization (IMO)
have resulted in a substantial reduction in the amount of SO2 emitted by
vessels crossing the oceans, particularly over the Atlantic and Pacific
oceans (Watson-Parris et al., 2022). Studies published before the
regulations went into effect had already postulated that they would have an
effect on cloud formation and direct forcing from the lack of sulfate
aerosols produced, with an overall small but non-zero global impact (Jin et
al., 2018). In the meantime, greenhouse gases concentrations keep rising,
and there is a growing perception amongst the general public and the
climate community that the latest extreme events observed have grown over
the last few years: 2023 has a high likelihood of being the warmest year
ever on record, while there have been record fire seasons in both Canada
and Hawaii and many regions in the Northern Hemisphere have observed
anomalously high sea surface temperature (SSTs), coupled with (and
partially driven by) a strong positive phase of ENSO. Discussions in the
news about whether some particular factors have contributed to this extreme
year are growing, and many have focused on the reduction in
sunlight-reflecting aerosols as a potential culprit.

Such questions are strongly tied with those around the opportunity to study
Sunlight Reflection Methods (SRM) as a climate intervention strategy that
may ameliorate the effects of climate change by reducing incoming sunlight,
perhaps using a thin layer of aerosols in the stratosphere, where they last
longer and are not as harmful to people. There is robust agreement over the
cooling potential of aerosols in the climate system: at the same time,
there is similar agreement over the health benefits of reducing aerosol
concentrations near human centers to improve public health. SRM by means of
stratospheric aerosol injections (SAI) might be a proposal that ties both
considerations, but in order to consider it seriously far more research is
needed to reduce uncertainties and understand how the climate system would
respond.

In this study, we use both a range of observation spanning surface air
temperatures (SAT), sea surface temperatures (SST) and top-of-atmosphere
Earth Energy Imbalance (EEI) and a large ensemble of simulations performed
with the Community Earth System Model (CESM2) (Simpson et al., 2023).
Firstly, we will use the CESM2 LENS to understand the detection of the
global signal and to attribute specific changes in regional climate,
coupling available simulations with new ones where the aerosol emissions
from shipping are quickly removed, as the LENS uses the Shared
Socioeconomic Pathway (SSP) 3-7.0, where shipping emissions continue. The
comparison of the two scenarios will provide a needed counterfactual that a
simple analysis of observational datasets, considering internal
variability, does not allow. However, the comparison of multiple
observational datasets (such as the Berkeley temperature record and various
reanalysis products such as ERA5) will also allow for a discussion of
statistical significance of the detected signal based on inherent
uncertainties in our knowledge of the climate system and internal climate
variability.

Secondly, we will expand this by simulating similar scenarios, but in which
the aerosols are not removed completely but moved to the stratosphere in
order to understand the projected differences between tropospheric and
stratospheric aerosols in terms of regional climatic impacts. This will
allow us to make more generalized conclusion around the issue of Climate
Intervention (CI), in particular the combined health and climatic benefits
of both removing aerosols from the troposphere, but adding them in the
stratosphere so that they can cool without impacting negatively on surface
air quality. This way of thinking about climate intervention will highlight
the concept that CI should be thought of not as an addiction but as a
vertical re-distribution of a fraction of the tropospheric aerosols, so
that they can keep their benefit and reduce their negative impacts, and
will help the community gain a better understanding of the limits of
detectability for CI, which can better inform future governance discussions
around outdoor tests.

Carbon Cycle Response to Stratospheric Aerosol Injection With Multiple
Temperature Stabilization Targets and Strategies
<https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2024EF004474>

Zhao, M., Cao, L., Visioni, D., & MacMartin, D. G. (2024). Carbon cycle
response to stratospheric aerosol injection with multiple temperature
stabilization targets and strategies. *Earth's Future*, *12*(6),
e2024EF004474.

*Abstract*

We analyze the global carbon cycle response to a set of stratospheric
aerosol injection (SAI) simulations performed by the CESM2(WACCM6-MA)
model. The simulations are performed under the specified SSP2-4.5 CO2
concentration pathway. It is found that both the temperature stabilization
target and the SO2 injection strategy have important effects on the global
carbon sink. Relative to the SSP2-4.5 scenario, averaged over the last 20
years of our simulations (year 2050–2069), simultaneous multi-location SO2
injection causes an increase in cumulative land carbon uptake of 45 and 23
PgC, and an increase in cumulative ocean carbon uptake of 6 and 2 PgC for
temperature stabilization targets of 0.5°C and 1.5°C respectively. For a
temperature stabilization target of 1.0°C, SO2 injections increase land and
ocean carbon sinks by 22–42 PgC and 4–7 PgC, respectively, depending on the
strategies of SO2 injections (low latitude, mid-to-high latitude, and
multi-objective injection). Relative to SSP2-4.5, by year 2069, SAI
increases diagnosed cumulative CO2 emissions by 25–53 PgC (3%–6%), implying
a decrease in atmospheric CO2 if SO2 injections were performed under a
prescribed CO2 emission pathway. Stratospheric SO2 injections slow
permafrost thaw, but do not restore permafrost to the previous extent at
the same warming level for all injection strategies. An abrupt termination
of SO2 injection weakens both the ocean and land carbon sink, and causes a
rapid decline of permafrost extent. A gradual phaseout of SO2 injection
slows sharp decline of permafrost and delays the rebound of carbon sink.

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WEB POSTSNew discovery reveals that ocean algae unexpectedly help cool the
Earth
<https://phys.org/news/2024-06-discovery-reveals-ocean-algae-unexpectedly.html>
(Phys.Org)This London non-profit is now one of the biggest backers of
geoengineering research — Plus, Simons, EDF and a new venture backed by
Meta’s former CTO are poised to pour tens of millions more into the
controversial field
<https://www.technologyreview.com/2024/06/14/1093778/foundations-are-lining-up-to-fund-geoengineering-research/>
(MIT *Technology* *Review*)Simons Foundation Funds 14 Projects Exploring
Earth-Cooling Techniques as Part of New International Research Program
<https://www.simonsfoundation.org/2024/06/12/simons-foundation-funds-14-projects-exploring-earth-cooling-techniques-as-part-of-new-international-research-program/>
(Simons Foundation)Environmental Group to Study Effects of Artificially
Cooling Earth
<https://www.nytimes.com/2024/06/10/climate/edf-solar-geoengineering-research.html>(The
New York Times)The Science And Ethics Of Solar Geoengineering
<https://salatainstitute.harvard.edu/the-science-and-ethics-of-solar-geoengineering/>
(Harvard)Can climate engineering be responsibly tested?
<https://thebarentsobserver.com/en/2024/06/not-ready-it-safe-alter-climate-reduce-global-warming-researchers-arctic-centre-lapland-try>
(The Barents Observer)Can mirrors help fight the threat of extreme heat?
<https://www.bbc.com/news/articles/c0kly57gl54o> (BBC)
[image: figure 4]
<https://substackcdn.com/image/fetch/f_auto,q_auto:good,fl_progressive:steep/https%3A%2F%2Fsubstack-post-media.s3.amazonaws.com%2Fpublic%2Fimages%2F9522b9b0-7d57-4b5f-ab75-baf0fc7c1e32_685x695.png>
New
discovery reveals that ocean algae unexpectedly help cool the Earth
<https://phys.org/news/2024-06-discovery-reveals-ocean-algae-unexpectedly.html>
(Phys.Org)
------------------------------
*REPORT*Insights Into Our Global Engagement Decision-making: Where We Go
And Why?
<https://sgdeliberation.org/publications/insights-into-our-global-engagement-decision-making-where-we-go-and-why/>
(DSG)
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*UPCOMING EVENTS**Governing Prometheus. Ethical Reflections On Risk &
Uncertainty In Solar Climate Engineering Research
<https://ethicsandtechnology.eu/calendar/governing-prometheus> | 19 June
2024 | TU Delft University**Fourteenth GeoMIP Workshop
<https://climate.envsci.rutgers.edu/GeoMIP/2024.html> | 10-12 July 2024 |
Ithaca, USA**RFF 2024 SRM Social Science Workshop: Cooperative vs.
Non-Cooperative Interventions
<https://docs.google.com/forms/d/1zE6Eo625cpEKZVbKwzDQSL4gxmnArmPsxtePJM-1SY0/viewform?edit_requested=true&gxid=-8203366>
| 19-20 September 2024 | Washington, DC.*

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------------------------------
*YOUTUBE VIDEOS*The Economics of Solar Radiative Management | Environmental
Defense Fund <https://www.youtube.com/watch?v=J5axhC5yAiw>Solar Climate
Intervention Virtual Symposium 11 (Dr. Claudia Wieners & Dr. Daniele
Visioni) | Solar Climate Intervention Talks
<https://www.youtube.com/watch?v=8qkwAGgZ2Kw>

"Solar Climate Intervention Virtual Symposium 11

Dr. Claudia Wieners (Utrecht University, Netherlands) : "Burning fossils
like hell and cooling in 2080 – what could possibly go wrong?
(Semi)-irreversible climate change under delayed stratospheric aerosol
injection."

Dr. Daniele Visioni (Cornell University, USA) : "Assessing sunlight
reflection methods on the international stage: what does it mean and where
are we? A perspective between science and politics."

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