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: Joughin, I., Smith, B. E., Shean, D. E., Floricioiu, D.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/tc-8-209-2014
https://tc.copernicus.org/articles/8/209/2014/
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author Joughin, I.
Smith, B. E.
Shean, D. E.
Floricioiu, D.
author_facet Joughin, I.
Smith, B. E.
Shean, D. E.
Floricioiu, D.
author_sort Joughin, I.
collection Copernicus Publications: E-Journals
container_issue 1
container_start_page 209
container_title The Cryosphere
container_volume 8
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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spelling ftcopernicus:oai:publications.copernicus.org:tc22549 2025-01-16T22:45:51+00:00 Brief Communication: Further summer speedup of Jakobshavn Isbræ Joughin, I. Smith, B. E. Shean, D. E. Floricioiu, D. 2018-09-27 application/pdf https://doi.org/10.5194/tc-8-209-2014 https://tc.copernicus.org/articles/8/209/2014/ eng eng doi:10.5194/tc-8-209-2014 https://tc.copernicus.org/articles/8/209/2014/ eISSN: 1994-0424 Text 2018 ftcopernicus https://doi.org/10.5194/tc-8-209-2014 2020-07-20T16:25:11Z 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. Text Jakobshavn Jakobshavn isbræ Copernicus Publications: E-Journals Jakobshavn Isbræ ENVELOPE(-49.917,-49.917,69.167,69.167) The Cryosphere 8 1 209 214
spellingShingle Joughin, I.
Smith, B. E.
Shean, D. E.
Floricioiu, D.
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
url https://doi.org/10.5194/tc-8-209-2014
https://tc.copernicus.org/articles/8/209/2014/