North Atlantic Western Boundary Currents Are Intense Dissolved Organic Carbon Streams

In the North Atlantic, there are two main western boundary currents related to the Atlantic Meridional Overturning Circulation (AMOC): the Gulf Stream flowing northward and the Deep Western Boundary Current (DWBC) flowing southward. Here we analyze data from the OVIDE section (GO-SHIP A25 Portugal-G...

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Bibliographic Details
Published in:Frontiers in Marine Science
Main Authors: Marcos Fontela, Fiz F. Pérez, Herlé Mercier, Pascale Lherminier
Format: Article in Journal/Newspaper
Language:English
Published: Frontiers Media S.A. 2020
Subjects:
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Online Access:https://doi.org/10.3389/fmars.2020.593757
https://doaj.org/article/b735468389954331b840c04d3b2b4fb4