Show simple item record

dc.contributor.authorVåge, Kjetil
dc.contributor.authorMoore, George William Kent
dc.contributor.authorJónsson, Steingrímur
dc.contributor.authorValdimarsson, Héðinn
dc.date.accessioned2017-09-22T12:33:21Z
dc.date.available2017-09-22T12:33:21Z
dc.date.issued2015
dc.identifier.citationVåge K, Moore GWK, Jónsson S, Valdimarsson H. Water mass transformation in the Iceland Sea. Deep Sea Research Part I: Oceanographic Research Papers. 2015;101:98-109eng
dc.identifier.urihttp://hdl.handle.net/1956/16721
dc.description.abstractThe water mass transformation that takes place in the Iceland Sea during winter is investigated using historical hydrographic data and atmospheric reanalysis fields. Surface densities exceeding σθ ¼ 27:8 kg=m3, and hence of sufficient density to contribute to the lower limb of the Atlantic Meridional Overturning Circulation via the overflows across the Greenland-Scotland Ridge, exist throughout the interior Iceland Sea east of the Kolbeinsey Ridge at the end of winter. The deepest and densest mixed layers are found in the northwest Iceland Sea on the outskirts of the basin׳s cyclonic gyre, largely determined by stronger atmospheric forcing near the ice edge. Much of the accumulated wintertime heat loss in that region takes place during a few extreme cold air outbreak events. Only a small number of hydrographic profiles (2%) recorded mixed layers sufficiently dense to supply the deepest part of the North Icelandic Jet, a current along the slope off northern Iceland that advects overflow water into the Denmark Strait. However, low values of potential vorticity at depth indicate that waters of this density class may be ventilated more regularly than the direct observations of dense mixed layers in the sparse data set indicate. A sudden increase in the depth of this deep isopycnal around 1995 suggests that the supply of dense water to the North Icelandic Jet, and hence to the densest component of the Atlantic Meridional Overturning Circulation, may have diminished over the past 20 years. Concurrent reductions in the turbulent heat fluxes and wind stress curl over the Iceland Sea are consistent with a decrease in convective activity and a weakening of the cyclonic gyre, both of which could have caused the increase in depth of these dense waters.eng
dc.language.isoengeng
dc.publisherElseviereng
dc.rightsAttribution CC BY-NC-NDeng
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/eng
dc.subjectIceland Seaeng
dc.subjectOpen-ocean convectioneng
dc.subjectNorth Icelandic Jeteng
dc.subjectDenmark Strait Overflow Watereng
dc.subjectAtlantic Meridional Overturning Circulationeng
dc.subjectCold air outbreakeng
dc.titleWater mass transformation in the Iceland Seaeng
dc.typeJournal articleeng
dc.subject.nsiVDP::Matematikk og naturvitenskap: 400::Geofag: 450::Oseanografi: 452
dc.subject.nsiVDP::Mathematics and natural scienses: 400::Geosciences: 450::Oceanography: 452
dc.date.updated2017-08-25T11:16:59Z
dc.rights.holderCopyright 2015 Elsevier Ltd.eng
dc.type.versionacceptedVersioneng
bora.peerreviewedPeer reviewedeng
dc.type.documentJournal article
dc.identifier.cristinID1246621
dc.identifier.doi10.1016/j.dsr.2015.04.001eng
dc.source.issn0967-0637eng
dc.source.issn1879-0119eng
dc.relation.projectIDNorges forskningsråd: 231647
dc.relation.journalDeep Sea Research Part I: Oceanographic Research Papers


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record

Attribution CC BY-NC-ND
Except where otherwise noted, this item's license is described as Attribution CC BY-NC-ND