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 bottomā€attached dense plume (overflow). The amount and distribution of entrainment and mixing that the overflow encounters during its...

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Bibliographic Details
Main Authors: Ilker Fer, Gunnar Voet, Knut S. Seim, Bert Rudels, Katrin Latarius
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
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