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...
Published in: | Journal of Geophysical Research: Oceans |
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Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
AGU (American Geophysical Union)
2000
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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 |
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. |
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