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Sub-daily sea ice motion and deformation from RADARSAT observations

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dc.contributor.author Kwok, R. en_US
dc.contributor.author Cunningham, G. F. en_US
dc.date.accessioned 2004-09-16T23:52:53Z
dc.date.available 2004-09-16T23:52:53Z
dc.date.issued 2003-12 en_US
dc.identifier.citation Geophysical research letters v.30, n.23, 2218, doi:10.1029/2003GL018723 en_US
dc.identifier.citation Pasadena, CA, USA en_US
dc.identifier.clearanceno 03-2404 en_US
dc.identifier.uri http://hdl.handle.net/2014/7880
dc.description.abstract We find a persistent level of oscillatory sea ice motion and deformation, superimposed on the large-scale wind-driven field, in May 2002 (spring) and February 2003 (mid-winter), in the high Arctic over a region centered at approx.(85degreeN, 135degreeW). At this latitude, the RADARSAT wide-swath SAR coverage provides 4??equential observations every day, for ice motion retrieval, with a sampling interval at the orbital period of approx. 101 minutes. en_US
dc.format.extent 1229662 bytes
dc.format.mimetype application/pdf
dc.language.iso en_US
dc.subject.other ice motion ice mechanics oceanography en_US
dc.title Sub-daily sea ice motion and deformation from RADARSAT observations en_US


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