Increased oceanic dimethyl sulfide emissions in areas of sea ice retreat inferred from a Greenland ice core
Ocean phytoplankton are an important source of dimethyl sulfide, which influences marine cloud formation. Model studies suggest that declines in Arctic sea ice may lead to increased dimethyl sulfide emissions, however observational support is lacking. Here, we present a 55-year high-resolution ice c...
Published in: | Communications Earth & Environment |
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Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Subjects: | |
Online Access: | http://hdl.handle.net/2115/87619 https://doi.org/10.1038/s43247-022-00661-w |