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...
Published in: | Frontiers in Marine Science |
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Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Frontiers Media
2020
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Subjects: | |
Online Access: | http://hdl.handle.net/10400.1/14953 https://doi.org/10.3389/fmars.2020.593757 |