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dc.contributor.authorGarner, P.
dc.date.accessioned2019-05-13T13:22:08Z
dc.date.available2019-05-13T13:22:08Z
dc.date.issued2009
dc.identifier.citation

Gatner, P. (2009) 'Labrador Sea Water formation in the Irminger Basin and its dependence on the North Atlantic Oscillation', The Plymouth Student Scientist, p. 199-269.

en_US
dc.identifier.issn1754-2383
dc.identifier.urihttp://hdl.handle.net/10026.1/13878
dc.description.abstract

Historical temperature and salinity data from the Irminger basin were analysed to determine if Labrador Sea Water forms in the Irminger Basin and if deep convection in the region is dependent on the North Atlantic Oscillation. This was undertaken by analysing the Surface Mixed Layer depth during the Boreal winter (December-March) and comparing it to the North Atlantic Oscillation Index. We find there is evidence of LSW formation in the region and there is a weak to moderate correlation with the North Atlantic Oscillation Index.

en_US
dc.language.isoenen_US
dc.publisherUniversity of Plymouth
dc.rightsAttribution 3.0 United States*
dc.rights.urihttp://creativecommons.org/licenses/by/3.0/us/*
dc.subjectsalinityen_US
dc.subjectLabrador Sea Wateren_US
dc.subjectNorth Atlantic Oscillation Indexen_US
dc.subjectBoreal winteren_US
dc.subjectSurface Mixed Layeren_US
dc.subjectNorth Atlantic Oscillationen_US
dc.subjectIrminger Basinen_US
dc.subjectdeep convectionen_US
dc.subjectoceanen_US
dc.subjectmarine environmenten_US
dc.subjectseaen_US
dc.titleLabrador Sea Water formation in the Irminger Basin and its dependence on the North Atlantic Oscillationen_US
dc.typeArticle
plymouth.issue2
plymouth.volume2
plymouth.journalThe Plymouth Student Scientist


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Attribution 3.0 United States
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