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Recent increases in Arctic freshwater flux affects Labrador Sea convection and Atlantic overturning circulation
The Atlantic Meridional Overturning Circulation (AMOC) is an important component of ocean thermohaline circulation. Melting of Greenland's ice sheet is freshening the North Atlantic; however, whether the augmented freshwater flux is disrupting the AMOC is unclear. Dense Labrador Sea Water (LSW)...
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| Pubblicato in: | Nat Commun |
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| Autori principali: | , , , , , , , |
| Natura: | Artigo |
| Lingua: | Inglês |
| Pubblicazione: |
Nature Publishing Group
2016
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| Soggetti: | |
| Accesso online: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4736158/ https://ncbi.nlm.nih.gov/pubmed/26796579 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/ncomms10525 |
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