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Role of Greenland Freshwater Anomaly in the Recent Freshening of the Subpolar North Atlantic

The cumulative Greenland freshwater flux anomaly has exceeded 5,000 km(3) since the 1990s. The volume of this surplus freshwater is expected to cause substantial freshening in the North Atlantic. Analysis of hydrographic observations in the subpolar seas reveals freshening signals in the 2010s. The...

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Bibliografiska uppgifter
I publikationen:J Geophys Res Oceans
Huvudupphovsmän: Dukhovskoy, D. S., Yashayaev, I., Proshutinsky, A., Bamber, J. L., Bashmachnikov, I. L., Chassignet, E. P., Lee, C. M., Tedstone, A. J.
Materialtyp: Artigo
Språk:Inglês
Publicerad: John Wiley and Sons Inc. 2019
Ämnen:
Länkar:https://ncbi.nlm.nih.gov/pmc/articles/PMC6618073/
https://ncbi.nlm.nih.gov/pubmed/31341755
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1029/2018JC014686
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