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Weak response of oceanic dimethylsulfide to upper mixing shoaling induced by global warming
The solar radiation dose in the oceanic upper mixed layer (SRD) has recently been identified as the main climatic force driving global dimethylsulfide (DMS) dynamics and seasonality. Because DMS is suggested to exert a cooling effect on the earth radiative budget through its involvement in the forma...
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| Prif Awduron: | , , |
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| Fformat: | Artigo |
| Iaith: | Inglês |
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National Academy of Sciences
2007
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| Mynediad Ar-lein: | https://ncbi.nlm.nih.gov/pmc/articles/PMC2042152/ https://ncbi.nlm.nih.gov/pubmed/17901211 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.0700843104 |
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