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Brief Communication: On the magnitude and frequency of Khurdopin glacier surge events
The Cryosphere, Volume: 8, Issue: 2, Pages: 571 - 574
Swansea University Author:
Adrian Luckman
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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...
| Published in: | The Cryosphere |
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| ISSN: | 1994-0424 |
| Published: |
Copernicus GmbH
2014
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| Online Access: |
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| URI: | https://cronfa.swan.ac.uk/Record/cronfa21914 |
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2015-06-03T02:09:47Z |
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2024-11-14T11:22:58Z |
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cronfa21914 |
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SURis |
| fullrecord |
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2024-04-28T16:16:24.4967961 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 BGPS 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 Biosciences Geography and Physics School COLLEGE CODE BGPS 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 |
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008cb668b2671b653a88677f075799a9 |
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008cb668b2671b653a88677f075799a9_***_Adrian Luckman |
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Adrian Luckman |
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D. J. Quincey Adrian Luckman |
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Journal article |
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The Cryosphere |
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8 |
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571 |
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2014 |
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1994-0424 |
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10.5194/tc-8-571-2014 |
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Copernicus GmbH |
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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. |
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2014-04-03T03:37:50Z |
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11.096892 |

