Brief Communication: On the magnitude and frequency of Khurdopin glacier surge events

The return periods of Karakoram glacier surges are poorly quantified. Here, we present evidence of an historic surge of the Khurdopin Glacier that began in the mid-1970s and peaked in 1979. Measured surface displacements reached >5 km a−1, two orders of magnitude faster than during quiescence. Th...

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Published in:The Cryosphere
Main Authors: D. J. Quincey, A. Luckman
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2014
Subjects:
Online Access:https://doi.org/10.5194/tc-8-571-2014
http://www.the-cryosphere.net/8/571/2014/tc-8-571-2014.pdf
https://doaj.org/article/c21dbbaf5d20424a905a486f90eadafb
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author D. J. Quincey
A. Luckman
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A. Luckman
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container_start_page 571
container_title The Cryosphere
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description The return periods of Karakoram glacier surges are poorly quantified. Here, we present evidence of an historic surge of the Khurdopin Glacier that began in the mid-1970s and peaked in 1979. Measured surface displacements reached >5 km a−1, two orders of magnitude faster than during quiescence. The Khurdopin Glacier next surged in the late 1990s, equating to a return period of 20 years. Surge evolution in the two events shows remarkable similarity suggesting a common trigger. Surge activity in the Karakoram needs to be better understood if accurate mass balance assessments of Hindu-Kush–Karakoram–Himalaya glaciers are to be made.
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spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:c21dbbaf5d20424a905a486f90eadafb 2025-01-17T01:05:53+00:00 Brief Communication: On the magnitude and frequency of Khurdopin glacier surge events D. J. Quincey A. Luckman 2014-04-01 https://doi.org/10.5194/tc-8-571-2014 http://www.the-cryosphere.net/8/571/2014/tc-8-571-2014.pdf https://doaj.org/article/c21dbbaf5d20424a905a486f90eadafb en eng Copernicus Publications 1994-0416 1994-0424 doi:10.5194/tc-8-571-2014 http://www.the-cryosphere.net/8/571/2014/tc-8-571-2014.pdf https://doaj.org/article/c21dbbaf5d20424a905a486f90eadafb undefined The Cryosphere, Vol 8, Iss 2, Pp 571-574 (2014) geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2014 fttriple https://doi.org/10.5194/tc-8-571-2014 2023-01-22T18:02:34Z The return periods of Karakoram glacier surges are poorly quantified. Here, we present evidence of an historic surge of the Khurdopin Glacier that began in the mid-1970s and peaked in 1979. Measured surface displacements reached >5 km a−1, two orders of magnitude faster than during quiescence. The Khurdopin Glacier next surged in the late 1990s, equating to a return period of 20 years. Surge evolution in the two events shows remarkable similarity suggesting a common trigger. Surge activity in the Karakoram needs to be better understood if accurate mass balance assessments of Hindu-Kush–Karakoram–Himalaya glaciers are to be made. Article in Journal/Newspaper The Cryosphere Unknown The Cryosphere 8 2 571 574
spellingShingle geo
envir
D. J. Quincey
A. Luckman
Brief Communication: On the magnitude and frequency of Khurdopin glacier surge events
title Brief Communication: On the magnitude and frequency of Khurdopin glacier surge events
title_full Brief Communication: On the magnitude and frequency of Khurdopin glacier surge events
title_fullStr Brief Communication: On the magnitude and frequency of Khurdopin glacier surge events
title_full_unstemmed Brief Communication: On the magnitude and frequency of Khurdopin glacier surge events
title_short Brief Communication: On the magnitude and frequency of Khurdopin glacier surge events
title_sort brief communication: on the magnitude and frequency of khurdopin glacier surge events
topic geo
envir
topic_facet geo
envir
url https://doi.org/10.5194/tc-8-571-2014
http://www.the-cryosphere.net/8/571/2014/tc-8-571-2014.pdf
https://doaj.org/article/c21dbbaf5d20424a905a486f90eadafb