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Wind-driven and buoyancy-driven circulation in the subtropical North Atlantic Ocean

Continuous observations of ocean circulation at 26°N in the subtropical Atlantic Ocean have been made since April 2004 to quantify the strength and variability in the Atlantic Meridional overturning circulation (AMOC), in which warm, upper waters flow northward and colder deep waters below 1100 m de...

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Detalles Bibliográficos
Autor principal:	Bryden, Harry L.
Formato:	Online Artículo Texto
Lenguaje:	English
Publicado:	The Royal Society 2021
Materias:	Review Articles
Acceso en línea:	https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8655619/ https://www.ncbi.nlm.nih.gov/pubmed/35153601 http://dx.doi.org/10.1098/rspa.2021.0172

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