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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Bibliographic Details
Main Author: Rignot, E
Format: Article in Journal/Newspaper
Language:unknown
Published: eScholarship, University of California 1997
Subjects:
Astronomy & Astrophysics
Greenland
glacier
Ice Sheet
Online Access:https://escholarship.org/uc/item/4zt5s2qr
id ftcdlib:oai:escholarship.org/ark:/13030/qt4zt5s2qr
record_format openpolar
spelling 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

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