Blar i Institutt for marin teknikk på tidsskrift "Journal of Geophysical Research"
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Mixing in the stratified interface of the Faroe Bank Channel overflow: the role of transverse circulation and internal waves
(Journal article; Peer reviewed, 2011)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 ...