Ice discharge from north and northeast Greenland using ERS data
Ice discharge from north and northeast Greenland glaciers was calculated at the grounding line using ERS radar interferometry data acquired during the tandem phase. The resulting estimates exceed the production of icebergs at the glacier fronts by a factor 3.5. This large decrease in ice flux is att...
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1997
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ftcdlib:oai:escholarship.org/ark:/13030/qt4zt5s2qr 2023-05-15T16:21:05+02:00 Ice discharge from north and northeast Greenland using ERS data Rignot, E 815 - 818 1997-12-01 application/pdf https://escholarship.org/uc/item/4zt5s2qr unknown eScholarship, University of California qt4zt5s2qr https://escholarship.org/uc/item/4zt5s2qr CC-BY CC-BY European Space Agency, (Special Publication) ESA SP, vol 414, iss 414 PART 2 Astronomy & Astrophysics article 1997 ftcdlib 2021-06-20T14:23:08Z Ice discharge from north and northeast Greenland glaciers was calculated at the grounding line using ERS radar interferometry data acquired during the tandem phase. The resulting estimates exceed the production of icebergs at the glacier fronts by a factor 3.5. This large decrease in ice flux is attributed to extensive melting at the underside of the floating sections. When compared to the predicted grounding line ice discharge of an ice sheet in balance, the results show an excess 28 km3/yr of ice lost to the ocean. The north and northeast sectors of the Greenland Ice Sheet are therefore thinning and contributing positively to sea-level rise. Article in Journal/Newspaper glacier Greenland Ice Sheet University of California: eScholarship Greenland |
institution |
Open Polar |
collection |
University of California: eScholarship |
op_collection_id |
ftcdlib |
language |
unknown |
topic |
Astronomy & Astrophysics |
spellingShingle |
Astronomy & Astrophysics Rignot, E Ice discharge from north and northeast Greenland using ERS data |
topic_facet |
Astronomy & Astrophysics |
description |
Ice discharge from north and northeast Greenland glaciers was calculated at the grounding line using ERS radar interferometry data acquired during the tandem phase. The resulting estimates exceed the production of icebergs at the glacier fronts by a factor 3.5. This large decrease in ice flux is attributed to extensive melting at the underside of the floating sections. When compared to the predicted grounding line ice discharge of an ice sheet in balance, the results show an excess 28 km3/yr of ice lost to the ocean. The north and northeast sectors of the Greenland Ice Sheet are therefore thinning and contributing positively to sea-level rise. |
format |
Article in Journal/Newspaper |
author |
Rignot, E |
author_facet |
Rignot, E |
author_sort |
Rignot, E |
title |
Ice discharge from north and northeast Greenland using ERS data |
title_short |
Ice discharge from north and northeast Greenland using ERS data |
title_full |
Ice discharge from north and northeast Greenland using ERS data |
title_fullStr |
Ice discharge from north and northeast Greenland using ERS data |
title_full_unstemmed |
Ice discharge from north and northeast Greenland using ERS data |
title_sort |
ice discharge from north and northeast greenland using ers data |
publisher |
eScholarship, University of California |
publishDate |
1997 |
url |
https://escholarship.org/uc/item/4zt5s2qr |
op_coverage |
815 - 818 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
glacier Greenland Ice Sheet |
genre_facet |
glacier Greenland Ice Sheet |
op_source |
European Space Agency, (Special Publication) ESA SP, vol 414, iss 414 PART 2 |
op_relation |
qt4zt5s2qr https://escholarship.org/uc/item/4zt5s2qr |
op_rights |
CC-BY |
op_rightsnorm |
CC-BY |
_version_ |
1766009096876589056 |