In places such as the Greenland-Iceland-Norwegian sea, and the Arctic or Antarctic shelves, dense water is formed and flows down topography. As the density current flows down the topography, it entrains ambient fluid. This
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.615.7371 2023-05-15T14:00:16+02:00 The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.615.7371 http://www.cmmap.org/research/docs/feb07/vanroekel.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.615.7371 http://www.cmmap.org/research/docs/feb07/vanroekel.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.cmmap.org/research/docs/feb07/vanroekel.pdf text ftciteseerx 2016-01-08T14:44:04Z In places such as the Greenland-Iceland-Norwegian sea, and the Arctic or Antarctic shelves, dense water is formed and flows down topography. As the density current flows down the topography, it entrains ambient fluid. This Text Antarc* Antarctic Arctic Greenland Iceland Norwegian Sea Unknown Antarctic Arctic Greenland Norwegian Sea |
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Open Polar |
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ftciteseerx |
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English |
description |
In places such as the Greenland-Iceland-Norwegian sea, and the Arctic or Antarctic shelves, dense water is formed and flows down topography. As the density current flows down the topography, it entrains ambient fluid. This |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.615.7371 http://www.cmmap.org/research/docs/feb07/vanroekel.pdf |
geographic |
Antarctic Arctic Greenland Norwegian Sea |
geographic_facet |
Antarctic Arctic Greenland Norwegian Sea |
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Antarc* Antarctic Arctic Greenland Iceland Norwegian Sea |
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Antarc* Antarctic Arctic Greenland Iceland Norwegian Sea |
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http://www.cmmap.org/research/docs/feb07/vanroekel.pdf |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.615.7371 http://www.cmmap.org/research/docs/feb07/vanroekel.pdf |
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