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Changes in the Norwegian Sea deep water

dc.contributor.authorØsterhus, Svein
dc.contributor.authorBlindheim, Johan
dc.contributor.authorTurrell, William R.
dc.contributor.authorHansen, Bogi
dc.contributor.authorvan Bennekom, Aleido Johannes
dc.date.accessioned2012-09-28T12:16:11Z
dc.date.available2012-09-28T12:16:11Z
dc.date.issued1996
dc.identifier.citationThis report is not to be cited without prior reference to the authorsno_NO
dc.identifier.urihttp://hdl.handle.net/11250/105637
dc.description.abstractThis paper deals with observed changes in the Norwegian Sea Deep Water (NSDW) after the cessation of bottom water formation in the Greenland Sea. Current measurements indicate that the deep water flow from the Greenland Sea to the Norwegian Sea has reversed. The Deep Water in the Norwegian Sea is warming in the entire layer below 1000m depth and down to the bottom. The thickness of the adiabatic layer is decreasing. The salinity of the homohaline layer is constant but the thickness is decreasing. The overflow water in the Faroe-Shetland Channel is freshening.no_NO
dc.language.isoengno_NO
dc.publisherICESno_NO
dc.relation.ispartofseriesICES CM Documents;1996/O:11
dc.subjectcurrent measurementsno_NO
dc.subjectstrømmålingerno_NO
dc.subjecthydrographyno_NO
dc.subjecthydrografino_NO
dc.subjectmonitoringno_NO
dc.subjectovervåkningno_NO
dc.subjectsalinityno_NO
dc.subjectsalinitetno_NO
dc.titleChanges in the Norwegian Sea deep waterno_NO
dc.typeWorking paperno_NO
dc.subject.nsiVDP::Mathematics and natural science: 400::Zoology and botany: 480::Marine biology: 497no_NO
dc.subject.nsiVDP::Mathematics and natural science: 400::Geosciences: 450::Oceanography: 452no_NO
dc.source.pagenumber4 s.no_NO


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