Show simple item record

Files in this item

Thumbnail

Item metadata

dc.contributor.authorArthun, Marius
dc.contributor.authorNicholls, Keith
dc.contributor.authorBoehme, Lars
dc.date.accessioned2013-08-01T23:50:04Z
dc.date.available2013-08-01T23:50:04Z
dc.date.issued2013-02
dc.identifier.citationArthun , M , Nicholls , K & Boehme , L 2013 , ' Wintertime water mass modification near an Antarctic Ice Shelf front ' Journal of Physical Oceanography , vol. 43 , no. 2 , pp. 359-365 . https://doi.org/10.1175/JPO-D-12-0186.1en
dc.identifier.issn0022-3670
dc.identifier.otherPURE: 27672043
dc.identifier.otherPURE UUID: e6a3f07c-cc81-42f9-98bb-c4cc9bcb93d1
dc.identifier.otherScopus: 84875549662
dc.identifier.urihttp://hdl.handle.net/10023/3903
dc.description.abstractUnder ice measurements by seals carrying a miniaturized conductivity–temperature–depth (CTD) instrument fill an important gap in existing observations. Here we present data from an instrumented Weddell seal that spent 8 consecutive months (February–September) for aging in close proximity to Filchner Ice Shelf, thus providing detailed information about the evolution of mixed layer hydrography during the austral autumn and winter. The resultant time series of hydrography shows strong seasonal water mass modification, dominated by an upper–ocean (0–300 m) salinity increase of 0.31, corresponding to 3.1 m sea ice growth, and the development of a 500 m thick winter mixed layer. Observations furthermore highlight a gradual salinity increase in a slow (3–5 cms−1 ) southward flow on the continental shelf, to wards the site, and suggest that the inferred ice production is better considered as a regional average rather than being purely local. No clear seasonality is observed in the properties of the underlying Ice Shelf Water.en
dc.language.isoeng
dc.relation.ispartofJournal of Physical Oceanographyen
dc.rights© 2013 American Meteorological Societyen
dc.subjectAntarcticaen
dc.subjectContinental shelf/slopeen
dc.subjectSea iceen
dc.subjectSouthern Oceanen
dc.subjectMixed layeren
dc.subjectIn situ oceanic observationsen
dc.subjectGC Oceanographyen
dc.subject.lccGCen
dc.titleWintertime water mass modification near an Antarctic Ice Shelf fronten
dc.typeJournal articleen
dc.description.versionPublisher PDFen
dc.contributor.institutionUniversity of St Andrews. School of Biologyen
dc.contributor.institutionUniversity of St Andrews. Scottish Oceans Instituteen
dc.contributor.institutionUniversity of St Andrews. Marine Alliance for Science & Technology Scotlanden
dc.contributor.institutionUniversity of St Andrews. Sea Mammal Research Uniten
dc.identifier.doihttps://doi.org/10.1175/JPO-D-12-0186.1
dc.description.statusPeer revieweden
dc.date.embargoedUntil02-08-20
dc.identifier.urlhttp://journals.ametsoc.org/doi/full/10.1175/JPO-D-12-0186.1


This item appears in the following Collection(s)

Show simple item record