Brief Communication: Further summer speedup of Jakobshavn Isbræ

We have extended the record of flow speed on Jakobshavn Isbræ through the summer of 2013. These new data reveal large seasonal speedups, 30 to 50% greater than previous summers. At a point a few kilometres inland from the terminus, the mean annual speed for 2012 is nearly three times as great as tha...

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Main Authors: I. Joughin, B. E. Smith, D. E. Shean, D. Floricioiu
Format: Article
Language:English
Published: Copernicus Publications 2014-02-01
Series:The Cryosphere
Online Access:http://www.the-cryosphere.net/8/209/2014/tc-8-209-2014.pdf
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spelling doaj-06a181843e834498bf61d9f500fb3b7d2020-11-25T00:35:12ZengCopernicus PublicationsThe Cryosphere1994-04161994-04242014-02-018120921410.5194/tc-8-209-2014Brief Communication: Further summer speedup of Jakobshavn IsbræI. Joughin0B. E. Smith1D. E. Shean2D. Floricioiu3Polar Science Center, Applied Physics Lab, University of Washington, 1013 NE 40th St., Seattle, WA 98105-6698, USAPolar Science Center, Applied Physics Lab, University of Washington, 1013 NE 40th St., Seattle, WA 98105-6698, USAPolar Science Center, Applied Physics Lab, University of Washington, 1013 NE 40th St., Seattle, WA 98105-6698, USAGerman Aerospace Center (DLR), Remote Sensing Technology Institute, SAR Signal Processing, Muenchenerstr. 20, 82230 Wessling, GermanyWe have extended the record of flow speed on Jakobshavn Isbræ through the summer of 2013. These new data reveal large seasonal speedups, 30 to 50% greater than previous summers. At a point a few kilometres inland from the terminus, the mean annual speed for 2012 is nearly three times as great as that in the mid-1990s, while the peak summer speeds are more than a factor of four greater. These speeds were achieved as the glacier terminus appears to have retreated to the bottom of an over-deepened basin with a depth of ~ 1300 m below sea level. The terminus is likely to reach the deepest section of the trough within a few decades, after which it could rapidly retreat to the shallower regions ~ 50 km farther upstream, potentially by the end of this century.http://www.the-cryosphere.net/8/209/2014/tc-8-209-2014.pdf
collection DOAJ
language English
format Article
sources DOAJ
author I. Joughin
B. E. Smith
D. E. Shean
D. Floricioiu
spellingShingle I. Joughin
B. E. Smith
D. E. Shean
D. Floricioiu
Brief Communication: Further summer speedup of Jakobshavn Isbræ
The Cryosphere
author_facet I. Joughin
B. E. Smith
D. E. Shean
D. Floricioiu
author_sort I. Joughin
title Brief Communication: Further summer speedup of Jakobshavn Isbræ
title_short Brief Communication: Further summer speedup of Jakobshavn Isbræ
title_full Brief Communication: Further summer speedup of Jakobshavn Isbræ
title_fullStr Brief Communication: Further summer speedup of Jakobshavn Isbræ
title_full_unstemmed Brief Communication: Further summer speedup of Jakobshavn Isbræ
title_sort brief communication: further summer speedup of jakobshavn isbræ
publisher Copernicus Publications
series The Cryosphere
issn 1994-0416
1994-0424
publishDate 2014-02-01
description We have extended the record of flow speed on Jakobshavn Isbræ through the summer of 2013. These new data reveal large seasonal speedups, 30 to 50% greater than previous summers. At a point a few kilometres inland from the terminus, the mean annual speed for 2012 is nearly three times as great as that in the mid-1990s, while the peak summer speeds are more than a factor of four greater. These speeds were achieved as the glacier terminus appears to have retreated to the bottom of an over-deepened basin with a depth of ~ 1300 m below sea level. The terminus is likely to reach the deepest section of the trough within a few decades, after which it could rapidly retreat to the shallower regions ~ 50 km farther upstream, potentially by the end of this century.
url http://www.the-cryosphere.net/8/209/2014/tc-8-209-2014.pdf
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