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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| Format: | Text |
| Language: | English |
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.615.7371 http://www.cmmap.org/research/docs/feb07/vanroekel.pdf |
| Summary: | 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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