Here for Full Article Intense mixing of the Faroe Bank Channel overflow
[1] The continuous, swift flow of cold water across the sill of the Faroe Bank Channel, the deepest passage from the Nordic Seas to the North Atlantic Ocean, forms a bottomāattached dense plume (overflow). The amount and distribution of entrainment and mixing that the overflow encounters during its...
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Format: | Text |
Language: | English |
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.689.7567 http://folk.uib.no/ngfif/Reprints/Fer_etal_GRL10.pdf |