On the relationship between dense water formation and the “Meridional Overturning Cell” in the North Atlantic Ocean
We analyze the three-dimensional structure of the Meridional Overturning Cell (MOC) in a numerical model of the North Atlantic and Arctic Oceans. The MOC is found to consist of several downward branches: some associated with dense water formation driven by surface buoyancy forcing (Labrador Sea, nor...
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Veröffentlicht in: | Deep-sea research. Part I, Oceanographic research papers Oceanographic research papers, 1999-05, Vol.46 (5), p.877-894 |
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Format: | Artikel |
Sprache: | eng |
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