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...

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Bibliographic Details
Published in:Journal of Geophysical Research: Oceans
Main Authors: Seim, Knut Sponheim, Fer, Ilker
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union (AGU) 2011
Subjects:
Online Access:http://hdl.handle.net/11250/2460483
https://doi.org/10.1029/2010JC006805