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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Detalhes bibliográficos
Autor principal: Fontela, Marcos (author)
Outros Autores: Pérez, Fiz F. (author), Mercier, Herlé (author), Lherminier, Pascale (author)
Formato: article
Idioma:eng
Publicado em: 2021
Assuntos:
North Atlantic
Atlantic meridional overturning circulation
Dissolved organic carbon
Carbon budget
Biogeochemistry
Carbon dioxide
Texto completo:http://hdl.handle.net/10400.1/14953
País:Portugal
Oai:oai:sapientia.ualg.pt:10400.1/14953

Texto Completo

http://hdl.handle.net/10400.1/14953

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