Inland thinning of the Amundsen Sea sector, West Antarctica. Geohys
the Amundsen Sea (AS) sector of Western Antarctica. Here we use satellite radar altimetry and interferometry to show that a rapid thinning of ice has occurred within the fastest flowing sections of all AS outlet glaciers. The pattern of thinning extends to distances greater than 150 km inland. Betwe...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.530.4089 2023-05-15T13:23:40+02:00 Inland thinning of the Amundsen Sea sector, West Antarctica. Geohys Andrew Shepherd Duncan J. Wingham Justin A. D. Mansley The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.530.4089 http://www.cpom.org/research/aps-grl.pdf en eng Adv http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.530.4089 http://www.cpom.org/research/aps-grl.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.cpom.org/research/aps-grl.pdf text ftciteseerx 2016-01-08T10:35:00Z the Amundsen Sea (AS) sector of Western Antarctica. Here we use satellite radar altimetry and interferometry to show that a rapid thinning of ice has occurred within the fastest flowing sections of all AS outlet glaciers. The pattern of thinning extends to distances greater than 150 km inland. Between 1991 and 2001, the TG and SG thinned by more than 25 and 45 m at their grounding lines, and a total of 154 ± 16 km3 of ice (or 0.43 mm of eustatic sea level rise) was lost from the AS sector glaciers to the ocean. We show that the thickness changes may have caused the PIG, TG, and SG to retreat inland by over 8, 4, and 7 km respectively, in line with independent estimates of grounding line migration. INDEX TERMS: 1827 Text Amundsen Sea Antarc* Antarctica West Antarctica Unknown Amundsen Sea West Antarctica |
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ftciteseerx |
language |
English |
description |
the Amundsen Sea (AS) sector of Western Antarctica. Here we use satellite radar altimetry and interferometry to show that a rapid thinning of ice has occurred within the fastest flowing sections of all AS outlet glaciers. The pattern of thinning extends to distances greater than 150 km inland. Between 1991 and 2001, the TG and SG thinned by more than 25 and 45 m at their grounding lines, and a total of 154 ± 16 km3 of ice (or 0.43 mm of eustatic sea level rise) was lost from the AS sector glaciers to the ocean. We show that the thickness changes may have caused the PIG, TG, and SG to retreat inland by over 8, 4, and 7 km respectively, in line with independent estimates of grounding line migration. INDEX TERMS: 1827 |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Andrew Shepherd Duncan J. Wingham Justin A. D. Mansley |
spellingShingle |
Andrew Shepherd Duncan J. Wingham Justin A. D. Mansley Inland thinning of the Amundsen Sea sector, West Antarctica. Geohys |
author_facet |
Andrew Shepherd Duncan J. Wingham Justin A. D. Mansley |
author_sort |
Andrew Shepherd |
title |
Inland thinning of the Amundsen Sea sector, West Antarctica. Geohys |
title_short |
Inland thinning of the Amundsen Sea sector, West Antarctica. Geohys |
title_full |
Inland thinning of the Amundsen Sea sector, West Antarctica. Geohys |
title_fullStr |
Inland thinning of the Amundsen Sea sector, West Antarctica. Geohys |
title_full_unstemmed |
Inland thinning of the Amundsen Sea sector, West Antarctica. Geohys |
title_sort |
inland thinning of the amundsen sea sector, west antarctica. geohys |
publisher |
Adv |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.530.4089 http://www.cpom.org/research/aps-grl.pdf |
geographic |
Amundsen Sea West Antarctica |
geographic_facet |
Amundsen Sea West Antarctica |
genre |
Amundsen Sea Antarc* Antarctica West Antarctica |
genre_facet |
Amundsen Sea Antarc* Antarctica West Antarctica |
op_source |
http://www.cpom.org/research/aps-grl.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.530.4089 http://www.cpom.org/research/aps-grl.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766373960421736448 |