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Process involved in the propagation of rifts across the Ronne Ice Shelf, near the region of Hemmen Ice Rise

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dc.contributor.author Larour, E. en_US
dc.contributor.author Rignot, E. en_US
dc.contributor.author Aubry, D. en_US
dc.date.accessioned 2004-09-17T07:06:36Z
dc.date.available 2004-09-17T07:06:36Z
dc.date.issued 2002-08-26 en_US
dc.identifier.citation International Glaciological Society Symposium en_US
dc.identifier.citation Chamonix Mont -Blac, France en_US
dc.identifier.clearanceno 02-1779 en_US
dc.identifier.uri http://hdl.handle.net/2014/9656
dc.description.abstract We use radar interferometric images collected by ERS-1 and Radarsat-1 to observe the rupture tip of rifts along Hemmen Ice Rise on the Ronne Ice Shelf, Antarctica. Interferograms generated in 1992 and 1997 allow us to observe the deformation of ice accumulated over respectively 9 and24 days. The results are an important step towards developing a better model of ice-shelf calving mechanism. en_US
dc.format.extent 4939242 bytes
dc.format.mimetype application/pdf
dc.language.iso en_US
dc.subject.other Hemmen Ice Rise Ronne Ice Shelf Antarctica calving icebergs rifts glaciers en_US
dc.title Process involved in the propagation of rifts across the Ronne Ice Shelf, near the region of Hemmen Ice Rise en_US


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