North and northeast Greenland ice discharge from satellite radar interferometry
Ice discharge from north and northeast Greenland calculated from satellite radar interferometry data of 14 outlet glaciers is 3.5 times that estimated from iceberg production. The satellite estimates, obtained at the grounding line of the outlet glaciers, differ from those obtained at the glacier fr...
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1997
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ftdtupubl:oai:pure.atira.dk:publications/bf826854-f3c3-4a90-b6fd-355507e68291 2024-05-19T07:40:41+00:00 North and northeast Greenland ice discharge from satellite radar interferometry Rignot, E.J. Gogineni, S.P. Krabill, W.B. Ekholm, Simon 1997 https://orbit.dtu.dk/en/publications/bf826854-f3c3-4a90-b6fd-355507e68291 eng eng https://orbit.dtu.dk/en/publications/bf826854-f3c3-4a90-b6fd-355507e68291 info:eu-repo/semantics/restrictedAccess Rignot , E J , Gogineni , S P , Krabill , W B & Ekholm , S 1997 , ' North and northeast Greenland ice discharge from satellite radar interferometry ' , Science , vol. 276 , no. 5314 , pp. 934-937 . article 1997 ftdtupubl 2024-04-24T00:24:29Z Ice discharge from north and northeast Greenland calculated from satellite radar interferometry data of 14 outlet glaciers is 3.5 times that estimated from iceberg production. The satellite estimates, obtained at the grounding line of the outlet glaciers, differ from those obtained at the glacier front, because basal melting is extensive at the underside of the floating glacier sections. The results suggest that the north and northeast parts of the Greenland ice sheet may be thinning and contributing positively to sea-level rise. Article in Journal/Newspaper glacier Greenland Ice Sheet Technical University of Denmark: DTU Orbit |
institution |
Open Polar |
collection |
Technical University of Denmark: DTU Orbit |
op_collection_id |
ftdtupubl |
language |
English |
description |
Ice discharge from north and northeast Greenland calculated from satellite radar interferometry data of 14 outlet glaciers is 3.5 times that estimated from iceberg production. The satellite estimates, obtained at the grounding line of the outlet glaciers, differ from those obtained at the glacier front, because basal melting is extensive at the underside of the floating glacier sections. The results suggest that the north and northeast parts of the Greenland ice sheet may be thinning and contributing positively to sea-level rise. |
format |
Article in Journal/Newspaper |
author |
Rignot, E.J. Gogineni, S.P. Krabill, W.B. Ekholm, Simon |
spellingShingle |
Rignot, E.J. Gogineni, S.P. Krabill, W.B. Ekholm, Simon North and northeast Greenland ice discharge from satellite radar interferometry |
author_facet |
Rignot, E.J. Gogineni, S.P. Krabill, W.B. Ekholm, Simon |
author_sort |
Rignot, E.J. |
title |
North and northeast Greenland ice discharge from satellite radar interferometry |
title_short |
North and northeast Greenland ice discharge from satellite radar interferometry |
title_full |
North and northeast Greenland ice discharge from satellite radar interferometry |
title_fullStr |
North and northeast Greenland ice discharge from satellite radar interferometry |
title_full_unstemmed |
North and northeast Greenland ice discharge from satellite radar interferometry |
title_sort |
north and northeast greenland ice discharge from satellite radar interferometry |
publishDate |
1997 |
url |
https://orbit.dtu.dk/en/publications/bf826854-f3c3-4a90-b6fd-355507e68291 |
genre |
glacier Greenland Ice Sheet |
genre_facet |
glacier Greenland Ice Sheet |
op_source |
Rignot , E J , Gogineni , S P , Krabill , W B & Ekholm , S 1997 , ' North and northeast Greenland ice discharge from satellite radar interferometry ' , Science , vol. 276 , no. 5314 , pp. 934-937 . |
op_relation |
https://orbit.dtu.dk/en/publications/bf826854-f3c3-4a90-b6fd-355507e68291 |
op_rights |
info:eu-repo/semantics/restrictedAccess |
_version_ |
1799480257688895488 |