Mixing in the stratified interface of the Faroe Bank Channel overflow: the role of transverse circulation and internal waves
The overflow of cold water across the Faroe Bank Channel sill is a significant volume flux of dense water to the North Atlantic Ocean. Using observations of hydrography, current and microstructure from a 1 week cruise and 2 month long time series from moored instruments, we address the role of trans...
Published in: | Journal of Geophysical Research: Oceans |
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Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
American Geophysical Union (AGU)
2011
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Subjects: | |
Online Access: | http://hdl.handle.net/11250/2460483 https://doi.org/10.1029/2010JC006805 |