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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Main Authors: Rignot, E.J., Gogineni, S.P., Krabill, W.B., Ekholm, Simon
Format: Article in Journal/Newspaper
Language:English
Published: 1997
Subjects:
Online Access:https://orbit.dtu.dk/en/publications/bf826854-f3c3-4a90-b6fd-355507e68291
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spelling 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
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