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Flow through Denmark Strait
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DOI：10.1029/2000JC900111.png)
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Abstract
En 中文
On the basis of hydrographic observations taken in the vicinity of Denmark Strait, a primitive equation model is used to investigate physical mechanisms that control the exchange through the strait. The dense water transport is topographically controlled and predictions by Whitehead [1998] and Killworth and McDonald [1993] are consistent with numerical model results. The distribution of temperature and thickness of the modeled plume is in good agreement with the high-resolution hydrographic data.
Keywords:
HYDRAULICALLY DRAINED FLOWS
STRATIFIED HYDRAULICS
ROTATING BASINS
OVERFLOW
MODEL
EDDIES
BOTTOM
WATER
FLUID
Journal
J
IF:
3.4
Papers:
1.1W
Citations:
4.4W
Organization
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