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

D. J. Quincey, Adrian Luckman Orcid Logo

The Cryosphere, Volume: 8, Issue: 2, Pages: 571 - 574

Swansea University Author: Adrian Luckman Orcid Logo

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DOI (Published version): 10.5194/tc-8-571-2014

Abstract

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 mid1970s and peaked in 1979. Measured surface displacements reached >5kma−1, two orders of magnitude faster than during quiescence. The K...

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Published in: The Cryosphere
ISSN: 1994-0424
Published: Copernicus GmbH 2014
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URI: https://cronfa.swan.ac.uk/Record/cronfa21914
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last_indexed 2019-05-31T22:15:03Z
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spelling v2 21914 2015-06-02 Brief Communication: On the magnitude and frequency of Khurdopin glacier surge events 008cb668b2671b653a88677f075799a9 0000-0002-9618-5905 Adrian Luckman Adrian Luckman true false 2015-06-02 SGE 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 mid1970s and peaked in 1979. Measured surface displacements reached >5kma−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. Journal Article The Cryosphere 8 2 571 574 Copernicus GmbH 1994-0424 3 4 2014 2014-04-03 10.5194/tc-8-571-2014 COLLEGE NANME Geography COLLEGE CODE SGE Swansea University 2024-04-28T16:16:24.4967961 2015-06-02T13:50:41.6073337 Faculty of Science and Engineering School of Biosciences, Geography and Physics - Geography D. J. Quincey 1 Adrian Luckman 0000-0002-9618-5905 2 0021914-15062015090126.pdf tc-8-571-2014.pdf 2015-06-15T09:01:26.5130000 Output 2167086 application/pdf Version of Record true 2015-06-15T00:00:00.0000000 Released under the terms of a Creative Commons Attribution 3.0 License (CC-BY). true
title Brief Communication: On the magnitude and frequency of Khurdopin glacier surge events
spellingShingle Brief Communication: On the magnitude and frequency of Khurdopin glacier surge events
Adrian Luckman
title_short 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_sort Brief Communication: On the magnitude and frequency of Khurdopin glacier surge events
author_id_str_mv 008cb668b2671b653a88677f075799a9
author_id_fullname_str_mv 008cb668b2671b653a88677f075799a9_***_Adrian Luckman
author Adrian Luckman
author2 D. J. Quincey
Adrian Luckman
format Journal article
container_title The Cryosphere
container_volume 8
container_issue 2
container_start_page 571
publishDate 2014
institution Swansea University
issn 1994-0424
doi_str_mv 10.5194/tc-8-571-2014
publisher Copernicus GmbH
college_str Faculty of Science and Engineering
hierarchytype
hierarchy_top_id facultyofscienceandengineering
hierarchy_top_title Faculty of Science and Engineering
hierarchy_parent_id facultyofscienceandengineering
hierarchy_parent_title Faculty of Science and Engineering
department_str School of Biosciences, Geography and Physics - Geography{{{_:::_}}}Faculty of Science and Engineering{{{_:::_}}}School of Biosciences, Geography and Physics - Geography
document_store_str 1
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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 mid1970s and peaked in 1979. Measured surface displacements reached >5kma−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.
published_date 2014-04-03T16:16:23Z
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