*Subscribe to the Solar Geoengineering Updates Newsletter here:* Solar Geoengineering Updates <https://solargeoengineeringupdates.substack.com?utm_source=substack&utm_campaign=publication_embed&utm_medium=email> Monthly news summaries about solar geoengineering. Links to scientific papers, news articles, jobs, podcasts, and videos. <https://solargeoengineeringupdates.substack.com?utm_source=substack&utm_campaign=publication_embed&utm_medium=email> By Andrew Lockley <https://solargeoengineeringupdates.substack.com?utm_source=substack&utm_campaign=publication_embed&utm_medium=email> *WEEKLY SUMMARY (22 JANUARY - 28 JANUARY 2024) <https://substack.com/app-link/publications/1346479/drafts/cb9b3cfc-a516-4367-b3ab-f864ca032617?publication_id=1346479&post_id=140935232&utm_source=post-email-title&utm_campaign=email-post-title&isFreemail=false>*Links to recent scientific papers, web posts, upcoming events, job opportunities, podcasts, and event recordings, etc. on Solar Radiation Management Technology. ------------------------------ *RESEARCH PAPERS*Quantifying the Impact of Internal Variability on the CESM2 Control Algorithm for Stratospheric Aerosol Injection <https://essopenarchive.org/users/558657/articles/697851-quantifying-the-impact-of-internal-variability-on-the-cesm2-control-algorithm-for-stratospheric-aerosol-injection>
Charlotte J Connolly, Emily M Prewett, Elizabeth A. Barnes, et al. (2024). Quantifying the Impact of Internal Variability on the CESM2 Control Algorithm for Stratospheric Aerosol Injection. ESS Open Archive.*Abstract*Earth system models are a powerful tool to simulate the response to hypothetical climate intervention strategies, such as stratospheric aerosol injection (SAI). Recent simulations of SAI implement tools from control theory, called “controllers”, to determine the quantity of aerosol to inject into the stratosphere to reach or maintain specified global temperature targets, such as limiting global warming to 1.5\textdegree C above pre-industrial temperatures. This work explores how internal (unforced) climate variability can impact controller-determined injection amounts using the Assessing Responses and Impacts of Solar climate intervention on the Earth system with Stratospheric Aerosol Injection (ARISE-SAI) simulations. Since the ARISE-SAI controller determines injection amounts by comparing global annual-mean surface temperature to predetermined temperature targets, internal variability that impacts temperature can impact the total injection amount as well. Using an offline version of the ARISE-SAI controller and data from CESM2 earth system model simulations, we quantify how internal climate variability and volcanic eruptions impact injection amounts. While idealized, this approach allows for the investigation of a large variety of climate states without additional simulations and can be used to attribute controller sensitivities to specific modes of internal variability. Deep Learning Aerosol-Cloud Interactions from Satellite Imagery <https://ojs.aaai.org/index.php/AAAI-SS/article/view/27664> Warburton, P., Shuler, K., & Patel, L. (2023). Deep Learning Aerosol-Cloud Interactions from Satellite Imagery. In *Proceedings of the AAAI Symposium Series* (Vol. 2, No. 1, pp. 159-165).*Abstract*Satellite imagery can detect a wealth of ship tracks, temporary cloud trails created via cloud seeding by the emitted aerosols of large ships, a phenomenon that cannot be directly reproduced by global climate models. Ship tracks are satellite-observable examples of aerosol-cloud interactions, processes that constitute the largest uncertainty in climate forcing predictions, and when observed are also examples of Marine Cloud Brightening (MCB), a potential climate intervention strategy. Leveraging the large amount of observed ship track data to enhance understanding of aerosol-cloud interactions and the potentials of MCB is hindered by the computational infeasiblity of characterization from expensive physical models. In this paper, we focus on utilizing a cheaper physics-informed advection-diffusion surrogate to accurately emulate ship track behavior. As an indication of aerosol-cloud interaction behavior, we focus on learning the spreading behavior of ship tracks, neatly encoded in the emulator's spatio-temporal diffusion field. We train a convolutional LSTM to accurately learn the spreading behavior of simulated and satellite-masked ship tracks and discuss its potential in larger scale studies. Low-temperature ice nucleation of sea spray and secondary marine aerosols under cirrus cloud conditions <https://acp.copernicus.org/articles/24/911/2024/> Patnaude, R., Moore, K., Perkins, R., Hill, T., DeMott, P., & Kreidenweis, S. (2023). Low Temperature Ice Nucleation of Sea Spray and Secondary Marine Aerosols under Cirrus Cloud Conditions. *EGUsphere*, *2023*, 1-22.*Abstract*Sea spray aerosols (SSAs) represent one of the most abundant aerosol types on a global scale and have been observed at all altitudes including the upper troposphere. SSA has been explored in recent years as a source of ice-nucleating particles (INPs) in cirrus clouds due to the ubiquity of cirrus clouds and the uncertainties in their radiative forcing. This study expands upon previous works on low-temperature ice nucleation of SSA by investigating the effects of atmospheric aging of SSA and the ice-nucleating activity of newly formed secondary marine aerosols (SMAs) using an oxidation flow reactor. Polydisperse aerosol distributions were generated from a marine aerosol reference tank (MART) filled with 120 L of real or artificial seawater and were dried to very low relative humidity to crystallize the salt constituents of SSA prior to their subsequent freezing, which was measured using a continuous flow diffusion chamber (CFDC). Results show that for primary SSA (pSSA), as well as aged SSA and SMA (aSSA+SMA) at temperatures >220 K, homogeneous conditions (92 %–97 % relative humidity with respect to water – RHw) were required to freeze 1 % of the particles. However, below 220 K, heterogeneous nucleation occurs for both pSSA and aSSA+SMA at much lower RHw, where up to 1 % of the aerosol population freezes between 75 % and 80 % RHw. Similarities between freezing behaviors of the pSSA and aSSA+SMA at all temperatures suggest that the contributions of condensed organics onto the pSSA or alteration of functional groups in pSSA via atmospheric aging did not hinder the major heterogeneous ice nucleation process at these cirrus temperatures, which have previously been shown to be dominated by the crystalline salts. Occurrence of a 1 % frozen fraction of SMA, generated in the absence of primary SSA, was observed at or near water saturation below 220 K, suggesting it is not an effective INP at cirrus temperatures, similar to findings in the literature on other organic aerosols. Thus, any SMA coatings on the pSSA would only decrease the ice nucleation behavior of pSSA if the organic components were able to significantly delay water uptake of the inorganic salts, and apparently this was not the case. Results from this study demonstrate the ability of lofted primary sea spray particles to remain an effective ice nucleator at cirrus temperatures, even after atmospheric aging has occurred over a period of days in the marine boundary layer prior to lofting. We were not able to address aging processes under upper-tropospheric conditions. The Potential Environmental and Climate Impacts of Stratospheric Aerosol Injection: A Review <https://pubs.rsc.org/en/content/articlelanding/2024/ea/d3ea00134b> Huynh, H. N., & McNeill, V. F. (2024). The Potential Environmental and Climate Impacts of Stratospheric Aerosol Injection: A Review. *Environmental Science: Atmospheres*.*Abstract*Given the rise in global mean temperature as a direct consequence of increasing levels of greenhouse gases (GHG) in the atmosphere, a variety of climate engineering approaches, including stratospheric aerosol injection (SAI), have been proposed. Often criticized as a distraction from global efforts towards reducing GHG emissions, SAI aims to increase the Earth’s albedo by seeding aerosols in the lower stratosphere. Inspired in part by observations of temporary cooling of the Earth’s surface following major volcanic eruptions which introduced significant loadings of sulfate particles into the stratosphere, SAI has been explored extensively in modeling studies. The cooling effect may be accompanied by other significant consequences including stratospheric heating, stratospheric ozone (O3) depletion, and reduced global mean precipitation. In order to understand the potential environmental and climate impacts of SAI, we review the state of the knowledge regarding these issues, starting from an aerosol science perspective. We summarize aerosol radiative properties and the role they play in defining the optimal chemical and physical aerosol characteristics for SAI, and their implications for lower stratospheric warming. We then review in depth the impacts of stratospheric aerosol heterogeneous chemistry on global O3 levels. We review SAI modeling studies as well as their uncertainties, in comparison to the observed environmental and climate impacts of volcanically derived sulfate aerosols, including impacts on global temperature, stratospheric warming, and hydrological cycle. We also discuss the current governance and economic considerations of the application of SAI and raise essential questions from both research and social standpoints that should be addressed before SAI is deployed for climate change mitigation. <https://acp.copernicus.org/articles/24/911/2024/> ------------------------------ WEB POSTSThe Future of Solar Geoengineering Research <https://www.resources.org/common-resources/the-future-of-solar-geoengineering-research/> (RFF)Degrees-funded scientists building North-South connections at the ICTP <https://www.degrees.ngo/degrees-funded-scientists-building-north-south-connections-at-ictp> (The Degrees Initiative)Funding awards for development of an African SRM Research Coalition <https://www.degrees.ngo/funding-for-development-of-an-african-srm-research-coalition/> (The Degrees Initiative) ------------------------------ *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* ------------------------------ YOUTUBE VIDEOSSolar radiation modification in the United States: A Discussion | Climate Overshoot Commission <https://www.youtube.com/watch?v=aM6B9AUrPR4> *“24 January 2024, Commissioner Frances Beinecke chaired a webinar with panelists Lloyd Whitman, Yashasvi Raj, Shuchi Talati, and Ted Parson.”* The Future of Climate Change: Solar Geoengineering and Carbon Management Explored | THE GEOSTRATA <https://www.youtube.com/watch?v=g349zBKOkVE> *“Dr. Talati is the founder of the Alliance for Just Deliberation on Solar Geoengineering, a global effort to elevate the voices of climate-vulnerable communities & nations in solar geoengineering decision-making. Our conversation focuses on policies that are required to build sustainable and equitable technological carbon removal at scale.”* Solar geoengineering - Mankind's New weapon to combat climate crisis | SGS MEDIA INC. <https://www.youtube.com/watch?v=OFFfWI0Ga3s> ------------------------------ *DEADLINES**Call for Papers: Special Collection-Towards a Risk-Risk-Assessment of Solar Radiation Modification <https://academic.oup.com/oocc/pages/solar-radiation-modification?login=false> | Deadline for manuscript submissions: 31 May 2024**The Climate Intervention Environmental Impact Fund (CIEIF) announced another round of three grants for the first half of 2024 with increased award amounts of $65,000 each <https://cieif.org/new-global-climate-restoration-fund-announces-first-grant-cycle/> | Application Deadline: 01 June 2024* ------------------------------ -- You received this message because you are subscribed to the Google Groups "geoengineering" group. 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