Articles | Volume 22, issue 8
https://doi.org/10.5194/acp-22-5223-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-22-5223-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
OCEANFILMS (Organic Compounds from Ecosystems to Aerosols: Natural Films and Interfaces via Langmuir Molecular Surfactants) sea spray organic aerosol emissions – implementation in a global climate model and impacts on clouds
Susannah M. Burrows
CORRESPONDING AUTHOR
Pacific Northwest National Laboratory, Richland, Washington, USA
Richard C. Easter
Pacific Northwest National Laboratory, Richland, Washington, USA
Xiaohong Liu
Texas A&M University, College Station, Texas, USA
Po-Lun Ma
Pacific Northwest National Laboratory, Richland, Washington, USA
Hailong Wang
Pacific Northwest National Laboratory, Richland, Washington, USA
Scott M. Elliott
Los Alamos National Laboratory, Los Alamos, New Mexico, USA
Balwinder Singh
Pacific Northwest National Laboratory, Richland, Washington, USA
Kai Zhang
Pacific Northwest National Laboratory, Richland, Washington, USA
Philip J. Rasch
Pacific Northwest National Laboratory, Richland, Washington, USA
Department of Atmospheric Sciences, University of Washington, Seattle, WA, USA
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Latest update: 16 Nov 2024
Short summary
Sea spray particles are composed of a mixture of salts and organic substances from oceanic microorganisms. In prior work, our team developed an approach connecting sea spray chemistry to ocean biology, called OCEANFILMS. Here we describe its implementation within an Earth system model, E3SM. We show that simulated sea spray chemistry is consistent with observed seasonal cycles and that sunlight reflected by simulated Southern Ocean clouds increases, consistent with analysis of satellite data.
Sea spray particles are composed of a mixture of salts and organic substances from oceanic...
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