Marine emissions of methanethiol increase aerosol cooling in the Southern Ocean

Ocean-emitted dimethyl sulfide (DMS) is a major source of climate-cooling aerosols. However, most of the marine biogenic sulfur cycling is not routed to DMS but to methanethiol (MeSH), another volatile whose reactivity has hitherto hampered measurements. Therefore, the global emissions and climate i...

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Bibliographic Details
Published in:Science Advances
Main Authors: Wohl, Charel, Villamayor, Julián, Galí, Martí, Mahajan, Anoop S., Fernández, Rafael P., Cuevas, Carlos A., Bossolasco, Adriana, Li, Qinyi, Kettle, Anthony J., Williams, Tara, Sarda-Esteve, Roland, Gros, Valérie, Simó, Rafel, Saiz-Lopez, Alfonso
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 2024
Subjects:
Southern Ocean
Online Access:https://doi.org/10.1126/sciadv.adq2465
https://www.science.org/doi/pdf/10.1126/sciadv.adq2465
Description
Summary:Ocean-emitted dimethyl sulfide (DMS) is a major source of climate-cooling aerosols. However, most of the marine biogenic sulfur cycling is not routed to DMS but to methanethiol (MeSH), another volatile whose reactivity has hitherto hampered measurements. Therefore, the global emissions and climate impact of MeSH remain unexplored. We compiled a database of seawater MeSH concentrations, identified their statistical predictors, and produced monthly fields of global marine MeSH emissions adding to DMS emissions. Implemented into a global chemistry-climate model, MeSH emissions increase the sulfate aerosol burden by 30 to 70% over the Southern Ocean and enhance the aerosol cooling effect while depleting atmospheric oxidants and increasing DMS lifetime and transport. Accounting for MeSH emissions reduces the radiative bias of current climate models in this climatically relevant region.

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