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*WEEKLY SUMMARY (06 NOVEMBER - 12 NOVEMBER 2023)*
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*DEADLINES**Call for Proposals-Grants for social science research on solar
radiation modification | Deadline: 13 December 2023
<https://link.sbstck.com/redirect/406a123d-1524-41ec-b2b9-486abcf28cdf?j=eyJ1IjoiMjJrMHl3In0.wQQsFypG52typ8FI2nhnJ8eUoUIIkdCkuhmzxNYKtgE>*
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*RESEARCH PAPERS*Change in wind energy potential under Solar Radiation
Modification—Conference Paper
<https://gfzpublic.gfz-potsdam.de/pubman/faces/ViewItemFullPage.jsp?itemId=item_5017452_1>

Baur, S., Terray, L., Séférian, R., & Sanderson, B. M. (2023). Change in
wind energy potential under Solar Radiation Modification. In *XXVIII
General Assembly of the International Union of Geodesy and Geophysics
(IUGG)*. GFZ German Research Centre for Geosciences.*Abstract*Solar
Radiation Management (SRM) is increasingly being discussed as a
hypothetical policy tool to reduce global and regional temperatures to
supplement conventional carbon mitigation measures. A crucial part of the
net-zero transition is the shift to renewable energy (RE) resources. Here,
we analyze the change in technical wind energy potential under solar- and
sulfate-forced SRM. Simulated output from the Earth System Model
CNRM-ESM2-1 for scenario-based experiments (GeoMIP G6 and ScenarioMIP
output) are used for the assessment. Preliminary results indicate some
regional and global differences in potential wind RE production capacity
between solar-forced SRM, sulfur-forced SRM and climate change without SRM
for relevant regions and seasons. This study gives an indication as to how
RE capacity, and therefore the potential to limit decarbonisation rates,
may be affected by SRM deployment.

Substantial Radiative Warming by an Inadvertent Geoengineering Experiment
from 2020 Fuel Regulations
<https://www.researchsquare.com/article/rs-3490826/v1>

Yuan, T., Song, H., Oreopoulos, L., Wood, R., Bian, H., Breen, K., ... &
Platnick, S. (2023). Substantial Radiative Warming by an Inadvertent
Geoengineering Experiment from 2020 Fuel Regulations.AbstractHuman
activities affect the Earth’s climate through modifying the composition of
the atmosphere, which then creates radiative forcing that drives climate
change 1. The warming effect of anthropogenic greenhouse gases has been
partially balanced by the cooling effect of anthropogenic aerosols 2. In
2020, fuel regulations abruptly reduced the emission of sulfur dioxide from
international shipping by more than 80%3 and created an inadvertent
geoengineering experiment4,5 with global scale. Here we show the regulation
leads to a radiative forcing of 0.12 Wm-2 averaged over the global ocean
using a combination of modeling and satellite data. The forcing is
estimated to effectively double the warming rate of global mean temperature
in this decade with strong spatiotemporal heterogeneity. The warming effect
contributes 50% to the measured increase in planetary heat uptake since
2020. The radiative forcing also has strong hemispheric contrast of 0.12
Wm-2 and contributes to the measured hemispheric contrast in absorbed solar
radiation, which has important implications for precipitation patterns. Our
result suggests marine cloud brightening may be a viable geoengineering
method in temporarily cooling the climate.

High sensitivity of summer temperatures to stratospheric sulfur loading
from volcanoes in the Northern Hemisphere
<https://www.pnas.org/doi/10.1073/pnas.2221810120>

Burke, A., Innes, H. M., Crick, L., Anchukaitis, K. J., Byrne, M. P.,
Hutchison, W., ... & Wilson, R. (2023). High sensitivity of summer
temperatures to stratospheric sulfur loading from volcanoes in the Northern
Hemisphere. *Proceedings of the National Academy of Sciences*, *120*(47),
e2221810120.*Abstract*The 540s, 1450s, and 1600s represent three of the
five coldest decades in the Common Era (CE). In each of these cases, the
cause of these cold pulses has been attributed to large volcanic eruptions.
However, the provenance of the eruption and magnitude of the volcanic
forcing remains uncertain. Here, we use high-resolution sulfur isotopes in
Greenland and Antarctic ice cores measured across these events to provide a
means of improving sulfur loading estimates for these eruptions. In each
case, the largest reconstructed tree-ring cooling is associated with an
extratropical eruption, and the high-altitude stratospheric sulfate loading
of these events is substantially smaller than previous estimates (by up to
a factor of two). These results suggest an increased sensitivity of the
reconstructed Northern Hemisphere summer temperature response to
extratropical eruptions. This highlights the importance of climate
feedbacks and processes that amplify and prolong the cooling signal from
high latitudes, such as changes in sea ice extent and ocean heat content.

Spaces of anthropogenic CO2 emissions compatible with planetary boundaries
<https://www.researchsquare.com/article/rs-3402213/v1>

Bossy, T., Gasser, T., Ciais, P., Tanaka, K., Lecocq, F., & Bousquet, P.
(2023). Spaces of anthropogenic CO2 emissions compatible with planetary
boundaries.*Abstract**The concept of planetary boundaries delineates the
Earth system’s limits within which humanity can sustainably prosper.**Here,
we introduce a new modelling framework to translate four climate-related
boundaries: global warming, ocean acidification, sea level rise, and Arctic
sea ice melt. Using a reduced-form model, we map a range of anthropogenic
CO2 emissions and removals pathways consistent with the boundaries,
optionally adding solar radiation management (SRM) measures to the picture.
Our framework estimates safety levels as probabilities to stay within the
boundaries considering the physical uncertainty of the Earth system.**If
CO2 emissions peak in 2030, net-zero CO2 is reached in 2100, CDR deployment
capacity is 10 PgC per year, and SRM is not allowed, remaining within the
global warming boundary is ensured with a safety level of 66%. This level
is 50% for the sea level rise or the Arctic sea ice boundary; it is 26% for
the ocean acidification boundary. When all four boundaries are considered
together, it drops to only 12%, indicating a complex interplay of planetary
boundaries in determining the safety level.**Our results suggest a need to
assess planetary boundaries holistically to develop sustainable future
strategies.*

Aerosol-Induced Closure of Marine Cloud Cells: Enhanced Effects in the
Presence of Precipitation
<https://egusphere.copernicus.org/preprints/2023/egusphere-2023-2416/>

Christensen, M. W., Wu, P., Varble, A. C., Xiao, H., & Fast, J. D. (2023).
Aerosol-Induced Closure of Marine Cloud Cells: Enhanced Effects in the
Presence of Precipitation. *EGUsphere*, *2023*, 1-35.*Abstract*The Weather
Research Forecasting (WRF) V4.2 model is configured within a Lagrangian
framework to quantify the impact of aerosols on evolving cloud fields.
Simulations employing realistic meteorological boundary conditions are
based on 10 case study days offering diverse meteorology during the Aerosol
and Cloud Experiments in the Eastern North Atlantic (ACE-ENA). Cloud and
aerosol retrievals in observations from aircraft measurements, ground-based
Atmosphere Radiation Measurement (ARM) data at Graciosa Island in the
Azores, and A-Train and geostationary satellites are in good agreement with
the simulations. Higher aerosol concentration leads to suppressed drizzle
and increased cloud water content. These changes lead to larger radiative
cooling rates at cloud top, enhanced vertical velocity variance, and
increased vertical and horizontal wind speed near the base of the
lower-tropospheric inversion. As a result, marine cloud cell area expands,
narrowing the gap between shallow clouds and increasing cloud optical
thickness, liquid water content, and the top-of-atmosphere outgoing
shortwave flux. While similar aerosol effects are observed in lightly to
non-raining clouds, they tend to be smaller by comparison. These results
show a strong link between cloud cell area expansion and the radiative
adjustments caused by liquid water path and cloud fraction changes. These
adjustments scale by 74 % and 51 %, respectively, relative to the Twomey
effect. Given the limitations of traditional global climate model
resolutions, addressing mesoscale cloud-state transitions at
kilometer-scale resolutions or higher should be of utmost importance in
accurately quantifying aerosol radiative forcing.

Injection strategy – a driver of atmospheric circulation and ozone response
to stratospheric aerosol geoengineering
<https://acp.copernicus.org/articles/23/13665/2023/>

Bednarz, E. M., Butler, A. H., Visioni, D., Zhang, Y., Kravitz, B., &
MacMartin, D. G. (2023). Injection strategy–a driver of atmospheric
circulation and ozone response to stratospheric aerosol
geoengineering. *Atmospheric
Chemistry and Physics*, *23*(21), 13665-13684.*Abstract*Despite offsetting
global mean surface temperature, various studies demonstrated that
stratospheric aerosol injection (SAI) could influence the recovery of
stratospheric ozone and have important impacts on stratospheric and
tropospheric circulation, thereby potentially playing an important role in
modulating regional and seasonal climate variability. However, so far, most
of the assessments of such an approach have come from climate model
simulations in which SO2 is injected only in a single location or a set of
locations.Here we use CESM2-WACCM6 SAI simulations under a comprehensive
set of SAI strategies achieving the same global mean surface temperature
with different locations and/or timing of injections, namely an equatorial
injection, an annual injection of equal amounts of SO2 at 15∘ N and 15∘ S,
an annual injection of equal amounts of SO2 at 30∘ N and 30∘ S, and a polar
strategy injecting SO2 at 60∘ N and 60∘ S only in spring in each hemisphere.We
demonstrate that despite achieving the same global mean surface
temperature, the different strategies result in contrastingly different
magnitudes of the aerosol-induced lower stratospheric warming,
stratospheric moistening, strengthening of stratospheric polar jets in both
hemispheres, and changes in the speed of the residual circulation. These
impacts tend to maximise under the equatorial injection strategy and become
smaller as the aerosols are injected away from the Equator into the
subtropics and higher latitudes. In conjunction with the differences in
direct radiative impacts at the surface, these different stratospheric
changes drive different impacts on the extratropical modes of variability
(Northern and Southern Annular modes), including important consequences on
the northern winter surface climate, and on the intensity of tropical
tropospheric Walker and Hadley circulations, which drive tropical
precipitation patterns. Finally, we demonstrate that the choice of
injection strategy also plays a first-order role in the future evolution of
stratospheric ozone under SAI throughout the globe. Overall, our results
contribute to an increased understanding of the fine interplay of various
radiative, dynamical, and chemical processes driving the atmospheric
circulation and ozone response to SAI and lay the foundation for designing
an optimal SAI strategy that could form a basis of future multi-model
intercomparisons.

<https://www.researchsquare.com/article/rs-3402213/v1>
------------------------------
REPORTSSolar geoengineering research & governance-Policy brief
<https://www.woodwellclimate.org/solar-geoengineering-research-governance/>Draft
decision: Stratospheric aerosol injection and protection of the ozone layer
(ver 1)
<https://ozone.unep.org/meetings/thirty-fifth-meeting-parties/contact-groups/informal-discussions-stratospheric-aerosol-injection/>
(United Nations Environment Program)The Solar Geoengineering Ecosystem: Key
Actors Across the Landscape of the Field, Wil Burns & Shuchi Talati
(November 2023)
<https://sgdeliberation.org/publications/the-solar-geoengineering-ecosystem-key-actors-across-the-landscape-of-the-field/>
<https://sgdeliberation.org/wp-content/uploads/2023/11/DSG-FCEA-Landscape-Report_Final.pdf>
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MEETING SUMMARY REPORTA New Era for the Geoengineering Model
Intercomparison Project (GeoMIP)
<https://climate.envsci.rutgers.edu/pdf/GeoMIP13ExeterBAMS.pdf>
<https://climate.envsci.rutgers.edu/pdf/GeoMIP13ExeterBAMS.pdf>
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*UPCOMING EVENTS**104th Annual Meeting by American Meteorological Society
<https://ams.confex.com/ams/104ANNUAL/meetingapp.cgi/Program/1743> | 28
January 2024 - 01 February 2023**Climate Engineering (GRS)
<https://www.grc.org/climate-engineering-grs-conference/2024/>| 17-18
February 2024**GRC Climate Engineering 2024
<https://www.grc.org/climate-engineering-conference/2024/>| 18-23 February
2024*
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PODCASTSC2GTalk: Should Global South scientists engage in solar radiation
modification research? with Inés Camilloni | Carnegie Climate Governance
Initiative (C2G)
<https://www.carnegiecouncil.org/media/series/c2g/global-south-scientists-solar-radiation-modification-research>

*“It is important for scientists from the Global South to be engaged in
research and discussions around solar radiation modification (SRM) because
its potential impacts would affect everyone, says Inés Camilloni from the
University of Buenos Aires. Researchers need to consider the risks of SRM
against the risks of a dangerously warming planet. More research is needed,
because the world currently does not know enough to make informed
decisions.**Dr. Camilloni is currently associate professor at the
Department of Atmospheric and Oceanic Sciences of the University of Buenos
Aires, senior researcher of the National Scientific and Technical Research
Council at the Center for Atmosphere and Ocean Research (CIMA) in
Argentina, and vice-chair of the Intergovernmental Panel on Climate Change
Working Group 1.”*

Climate Now Debates: Solar Radiation Management (SRM) | Climate Now

Climate Now Debates: Solar Radiation Management (SRM)

Climate Now

1:10:34
<https://podcasts.apple.com/us/podcast/climate-now-debates-solar-radiation-management-srm/id1565404483?i=1000633972266&uo=4>

*“Geoengineering refers to the intentional intervention in Earth processes
for the purpose of mitigating climate change. A controversial topic,
geoengineering is typically divided into two categories: carbon dioxide
removal and solar radiation management. This second category, also known as
SRM, made headlines this summer when the White House released a report that
“opened the door” to future research on the topic.**In principle, SRM
includes any technology that could be used to reflect some of the sun’s
energy from the Earth in order to decrease the amount of associated
heating, effectively cooling the planet. And while the study of SRM has
mostly been limited to the lab and to date no large-scale experiments have
been conducted, more people are calling for the idea to be explored further
as global warming increases. At the same time, others are saying the door
needs to remain shut, as the potential for unintended political, societal
and ecological side effects are just too great.**To help us understand why
- why is SRM being considered, and why are people concerned that it is
being considered, Climate Now brought together five experts – Professors
Frank Biermann (Utrecht Univ.), David Keith (Univ. Chicago), Chukwumerije
Okereke (Alex Ekwueme Federal Univ. Ndufu-Alike, Nigeria), Jennie Stephens
(Northeastern Univ.), and Claudia Wieners (Utrecht Univ.) – to debate the
merits and risks of examining SRM as a possible climate solution.”*

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YOUTUBE VIDEOS*C2GTalk: Should Global South scientists engage in solar
radiation modification research? | *C2G Carnegie Climate Governance
Initiative <https://www.youtube.com/watch?v=E2kZdRlU8_Q>

*“It is important for scientists from the Global South to be engaged in
research and discussions around SRM, because its potential impacts would
affect everyone, says Inés Camilloni from the University of Buenos Aires.
Researchers need to consider the risks of SRM against the risks of a
dangerously warming planet. More research is needed, because the world
currently does not know enough to make informed decisions.”*

*Webinar 24 | Solar Radiation Management with Harmattan over Southern West
Africa | Meteorological Virtual Seminar Series Ghana*
<https://www.youtube.com/watch?v=cRrXXjuSbEk>

*“Solar geoengineering is often discussed as a means to mitigate the
impacts and injustice of climate change by reducing its magnitude. However,
climate response to Solar Radiation Management simulation at a regional
scale remains uncertain. In addition, the potential effects of
geoengineering on temperature levels during the harmattan season in West
Africa are not well understood. This study aims to project how
geoengineering could impact harmattan temperatures by comparing current
temperature trends under moderate and high greenhouse gas emissions
scenarios (Representative Concentration Pathways 4.5 and 8.5) with and
without geoengineering. The findings suggest that if geoengineering
deployment cools the tropics during the harmattan season, it could
potentially increase the discomfort caused by the cold and dry conditions
that persist during the harmattan season, especially for those who are not
accustomed to the cold. Additionally, the study indicates that
geoengineering could offset the projected harmattan temperature reduction
that may occur by 2070 without intervention. These results highlight the
importance of considering the potential regional trade-offs that could
arise from implementing geoengineering strategies to offset warming during
the harmattan season in West Africa.”*

Climate Now Debates: Solar Radiation Management (SRM) | Climate Now
<https://www.youtube.com/watch?v=qpgfTcZYZNc>

*“Geoengineering refers to the intentional intervention in Earth processes
for the purpose of mitigating climate change. A controversial topic,
geoengineering is typically divided into two categories: carbon dioxide
removal and solar radiation management. This second category, also known as
SRM, made headlines this summer when the White House released a report that
“opened the door” to future research on the topic.”*

Solar Radiation Modification Youth Watch Launch Event at Climate Week NYC |
SRM Youth Watch <https://www.youtube.com/watch?v=Blk7-xo-TV4>

*“The Solar Radiation Modification Youth Watch (SRM YW) launch event aims
to bring together young people to discuss the need for strengthening
governance around solar radiation modification (SRM) whilst introducing and
launching the SRM YW platform.”*

*A virtual event: Global Dialogue on Climate Cooperation and Governance |
C2G Carnegie Climate Governance Initiative*
<https://www.youtube.com/watch?v=Ss1faZoAx7A>

*“A virtual event between the Institute for Sustainable Development Goals,
Tsinghua University (TUSDG), Center for Industrial Development and
Environmental Governance, Tsinghua University (CIDEG), and Carnegie Climate
Governance Initiative (C2G).”*

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