Flow through Denmark Strait

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 Killw...

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Bibliographic Details
Published in:Journal of Geophysical Research: Oceans
Main Authors: Käse, Rolf H., Oschlies, Andreas
Format: Article in Journal/Newspaper
Language:English
Published: AGU (American Geophysical Union) 2000
Subjects:
Online Access:https://oceanrep.geomar.de/id/eprint/1888/
https://oceanrep.geomar.de/id/eprint/1888/1/Kase00.pdf
https://doi.org/10.1029/2000JC900111
Description
Summary: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.