The presence and influence of glacier surging around the Geladandong ice caps, North East Tibetan Plateau

Many glaciers and ice caps on the Tibetan Plateau have retreated and lost mass in recent years in response to temperature increases, providing clear evidence of the impact of climate change on the region. There is increasing evidence that many of the glaciers on the Tibetan Plateau have also shown p...

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Main Authors: Owen King, Atanu Bhattacharya, Tobias Bolch
Format: Article
Language:English
Published: KeAi Communications Co., Ltd. 2021-06-01
Series:Advances in Climate Change Research
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S1674927821000721
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spelling doaj-1990c16e359842f787ed8d254662aead2021-07-23T04:48:05ZengKeAi Communications Co., Ltd.Advances in Climate Change Research1674-92782021-06-01123299312The presence and influence of glacier surging around the Geladandong ice caps, North East Tibetan PlateauOwen King0Atanu Bhattacharya1Tobias Bolch2Department of Geography and Sustainable Development, University of St Andrews, St Andrews, KY16 9AL, UK; Corresponding author.Department of Geography and Sustainable Development, University of St Andrews, St Andrews, KY16 9AL, UK; Department of Remote Sensing and GIS, JIS University, Kolkata, 700109, IndiaDepartment of Geography and Sustainable Development, University of St Andrews, St Andrews, KY16 9AL, UKMany glaciers and ice caps on the Tibetan Plateau have retreated and lost mass in recent years in response to temperature increases, providing clear evidence of the impact of climate change on the region. There is increasing evidence that many of the glaciers on the Tibetan Plateau have also shown periodically dynamic behaviour in the form of glacier surging and some even catastrophic collapse events. In this study, we examine the prevalence of glacier surging at the Geladandong ice caps, North East Tibetan Plateau, to better understand the role of surge events in the evolution of glacier mass loss budgets. Using glacier surface elevation change data over the period 1969–2018 and glacier surface velocity data from the ITS_LIVE dataset, we find that 19 outlet glaciers of the ice caps are of surge-type. Our multi-temporal measurements of glacier mass balance show that surge-type glacier mass budgets vary depending on the portion of the surge-cycle captured by geodetic data. At the regional level, pre- and post-surge glacier mass loss variability does not bias regional mass budget estimates, but enhanced, or suppressed, mass loss estimates are likely when small groups of glaciers are examined. Our results emphasise the importance of accurate surge-type glacier inventories and the need to maximise geodetic data coverage over glacierised regions known to contain surge-type glaciers.http://www.sciencedirect.com/science/article/pii/S1674927821000721Glacier surgeRemote sensingCorona KH-4Glacier mass balanceASTERTibetan Plateau
collection DOAJ
language English
format Article
sources DOAJ
author Owen King
Atanu Bhattacharya
Tobias Bolch
spellingShingle Owen King
Atanu Bhattacharya
Tobias Bolch
The presence and influence of glacier surging around the Geladandong ice caps, North East Tibetan Plateau
Advances in Climate Change Research
Glacier surge
Remote sensing
Corona KH-4
Glacier mass balance
ASTER
Tibetan Plateau
author_facet Owen King
Atanu Bhattacharya
Tobias Bolch
author_sort Owen King
title The presence and influence of glacier surging around the Geladandong ice caps, North East Tibetan Plateau
title_short The presence and influence of glacier surging around the Geladandong ice caps, North East Tibetan Plateau
title_full The presence and influence of glacier surging around the Geladandong ice caps, North East Tibetan Plateau
title_fullStr The presence and influence of glacier surging around the Geladandong ice caps, North East Tibetan Plateau
title_full_unstemmed The presence and influence of glacier surging around the Geladandong ice caps, North East Tibetan Plateau
title_sort presence and influence of glacier surging around the geladandong ice caps, north east tibetan plateau
publisher KeAi Communications Co., Ltd.
series Advances in Climate Change Research
issn 1674-9278
publishDate 2021-06-01
description Many glaciers and ice caps on the Tibetan Plateau have retreated and lost mass in recent years in response to temperature increases, providing clear evidence of the impact of climate change on the region. There is increasing evidence that many of the glaciers on the Tibetan Plateau have also shown periodically dynamic behaviour in the form of glacier surging and some even catastrophic collapse events. In this study, we examine the prevalence of glacier surging at the Geladandong ice caps, North East Tibetan Plateau, to better understand the role of surge events in the evolution of glacier mass loss budgets. Using glacier surface elevation change data over the period 1969–2018 and glacier surface velocity data from the ITS_LIVE dataset, we find that 19 outlet glaciers of the ice caps are of surge-type. Our multi-temporal measurements of glacier mass balance show that surge-type glacier mass budgets vary depending on the portion of the surge-cycle captured by geodetic data. At the regional level, pre- and post-surge glacier mass loss variability does not bias regional mass budget estimates, but enhanced, or suppressed, mass loss estimates are likely when small groups of glaciers are examined. Our results emphasise the importance of accurate surge-type glacier inventories and the need to maximise geodetic data coverage over glacierised regions known to contain surge-type glaciers.
topic Glacier surge
Remote sensing
Corona KH-4
Glacier mass balance
ASTER
Tibetan Plateau
url http://www.sciencedirect.com/science/article/pii/S1674927821000721
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