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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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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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The Royal Society
2021
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| 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 |