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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Detalhes bibliográficos
Publicado no:Nat Commun
Main Authors: Yang, Qian, Dixon, Timothy H., Myers, Paul G., Bonin, Jennifer, Chambers, Don, van den Broeke, M. R., Ribergaard, Mads H., Mortensen, John
Formato: Artigo
Idioma:Inglês
Publicado em: Nature Publishing Group 2016
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Article
Acesso em linha: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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