Vis enkel innførsel

dc.contributor.authorWidell, K.eng
dc.contributor.authorØsterhus, Sveineng
dc.contributor.authorGammelsrød, Toreng
dc.date.accessioned2004-08-11T08:39:28Zen_US
dc.date.accessioned2004-08-26T11:57:17Z
dc.date.available2004-08-11T08:39:28Zen_US
dc.date.available2004-08-26T11:57:17Z
dc.date.issued2003-10-04eng
dc.PublishedGeophysical Research Letters 30(19): 1982en_US
dc.identifier.issn0094-8276en_US
dc.identifier.urihttps://hdl.handle.net/1956/361
dc.description.abstractThe Fram Strait sea ice velocity was measured by means of a new method using moored Doppler Current Meters in the period 1996–2000. Almost 3 years of ice velocity observations near 79N 5W are analyzed. The average southward ice velocity was 0.16 m/s. The correlation between the ice velocity and the cross-strait sea level pressure (SLP) difference was R = 0.76 for daily means and R = 0.79 for monthly means. The same crossstrait SLP difference exhibits a positive trend since 1950 of 10% of the mean per decade. By a simple linear model we compute mean sea ice area flux to 850 000 km2/year for the period 1950–2000. Ice thickness, monitored by means of Upward Looking Sonars since 1990, is also discussed. The combined data gave a monthly ice volume flux of 200 km3 during the last decade with no significant trend.en_US
dc.format.extent17853 byteseng
dc.format.extent137 byteseng
dc.format.extent329778 byteseng
dc.format.mimetypetext/plaineng
dc.format.mimetypetext/plaineng
dc.format.mimetypeapplication/pdfeng
dc.language.isoengeng
dc.publisherAmerican Geophysical Unionen_US
dc.titleSea ice velocity in the Fram Strait monitored by moored instrumentsen_US
dc.typePeer reviewed
dc.typeJournal article
dc.description.versionpublishedVersionen_US
dc.rights.holderCopyright 2003 by the American Geophysical Unionen_US
dc.identifier.doihttps://doi.org/10.1029/2003gl018119
dc.source.journalGeophysical Research Letters
dc.source.4030
dc.source.1419


Tilhørende fil(er)

Thumbnail

Denne innførselen finnes i følgende samling(er)

Vis enkel innførsel