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dc.contributor.authorGeyer, Florianeng
dc.contributor.authorØsterhus, Sveineng
dc.contributor.authorHansen, Bogieng
dc.contributor.authorQuadfasel, D.eng
dc.date.accessioned2007-02-06T11:24:39Z
dc.date.available2007-02-06T11:24:39Z
dc.date.issued2006-12-23eng
dc.PublishedJournal of Geophysical Research 111(C12)
dc.identifier.issn0148-0227en_US
dc.identifier.issn2156-2202en_US
dc.identifier.urihttps://hdl.handle.net/1956/2086
dc.description.abstractThe Faroe Bank Channel (FBC) is the deepest connection between the Atlantic Ocean and the Nordic Seas. This work describes the dynamic properties of the plume of dense overflow water descending from the Faroe Bank Channel using time series data for velocity and temperature from a network of 25 moorings deployed west of the Faroe Bank Channel between July 1999 and February 2001. The cold water plume was identified using mean velocity and temperature data. A regular pattern of strong velocity and temperature oscillations with 88 ± 4 hours period was the most striking feature observed in the FBC overflow plume. These oscillations are initiated in a region where observations indicate supercritical conditions and compare well to recent model results for the FBC overflow plume by Ezer (2006).en_US
dc.format.extent1132574 byteseng
dc.format.mimetypeapplication/pdfeng
dc.language.isoengeng
dc.publisherAGUen_US
dc.titleObservations of highly regular oscillations in the overflow plume downstream of the Faroe Bank Channelen_US
dc.typePeer reviewed
dc.typeJournal article
dc.description.versionacceptedVersionen_US
dc.rights.holderCopyright 2006 by the American Geophysical Unionen_US
dc.identifier.doihttps://doi.org/10.1029/2006jc003693
dc.source.journalJournal of Geophysical Research
dc.source.40111
dc.source.14C12
dc.subject.nsiVDP::Matematikk og Naturvitenskap: 400nob


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