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Impacts of Shifts in Phytoplankton Community on Clouds and Climate via the Sulfur Cycle
2018
Global Biogeochemical Cycles
Dimethyl sulfide (DMS), primarily produced by marine organisms, contributes significantly to sulfate aerosol loading over the ocean after being oxidized in the atmosphere. In addition to exerting a direct radiative effect, the resulting aerosol particles act as cloud condensation nuclei, modulating cloud properties and extent, with impacts on atmospheric radiative transfer and climate. Thus, changes in pelagic ecosystems, such as phytoplankton physiology and community structure, may influence
doi:10.1029/2017gb005862
fatcat:bxei7d2khrervgsg7ggptrxp6q