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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Published in:The Cryosphere
Main Authors: I. Joughin, B. E. Smith, D. E. Shean, D. Floricioiu
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2014
Subjects:
Online Access:https://doi.org/10.5194/tc-8-209-2014
https://doaj.org/article/06a181843e834498bf61d9f500fb3b7d
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author I. Joughin
B. E. Smith
D. E. Shean
D. Floricioiu
author_facet I. Joughin
B. E. Smith
D. E. Shean
D. Floricioiu
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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.
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Jakobshavn isbræ
The Cryosphere
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https://doaj.org/article/06a181843e834498bf61d9f500fb3b7d
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spelling ftdoajarticles:oai:doaj.org/article:06a181843e834498bf61d9f500fb3b7d 2025-01-16T22:45:51+00:00 Brief Communication: Further summer speedup of Jakobshavn Isbræ I. Joughin B. E. Smith D. E. Shean D. Floricioiu 2014-02-01T00:00:00Z https://doi.org/10.5194/tc-8-209-2014 https://doaj.org/article/06a181843e834498bf61d9f500fb3b7d EN eng Copernicus Publications http://www.the-cryosphere.net/8/209/2014/tc-8-209-2014.pdf https://doaj.org/toc/1994-0416 https://doaj.org/toc/1994-0424 1994-0416 1994-0424 doi:10.5194/tc-8-209-2014 https://doaj.org/article/06a181843e834498bf61d9f500fb3b7d The Cryosphere, Vol 8, Iss 1, Pp 209-214 (2014) Environmental sciences GE1-350 Geology QE1-996.5 article 2014 ftdoajarticles https://doi.org/10.5194/tc-8-209-2014 2022-12-31T03:13:22Z 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. Article in Journal/Newspaper Jakobshavn Jakobshavn isbræ The Cryosphere Directory of Open Access Journals: DOAJ Articles Jakobshavn Isbræ ENVELOPE(-49.917,-49.917,69.167,69.167) The Cryosphere 8 1 209 214
spellingShingle Environmental sciences
GE1-350
Geology
QE1-996.5
I. Joughin
B. E. Smith
D. E. Shean
D. Floricioiu
Brief Communication: Further summer speedup of Jakobshavn Isbræ
title 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_short Brief Communication: Further summer speedup of Jakobshavn Isbræ
title_sort brief communication: further summer speedup of jakobshavn isbræ
topic Environmental sciences
GE1-350
Geology
QE1-996.5
topic_facet Environmental sciences
GE1-350
Geology
QE1-996.5
url https://doi.org/10.5194/tc-8-209-2014
https://doaj.org/article/06a181843e834498bf61d9f500fb3b7d