Glaciological and climatological drivers of heterogeneous glacier mass loss in the Tanggula Shan (Central-Eastern Tibetan Plateau), since the 1960s

Despite their extreme elevation, glaciers on the Tibetan Plateau are losing mass in response to atmospheric warming, the pattern of which purportedly reflects regional contrasts in climate. Here we examine the evolution of glaciers along ~500 km of the Tanggula Shan, Central-Eastern Tibetan Plateau....

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Main Authors: Owen King, Sajid Ghuffar, Atanu Bhattacharya, Ruzhen Yao, Tandong Yao, Tobias Bolch
Format: Article
Language:English
Published: Cambridge University Press 2023-10-01
Series:Journal of Glaciology
Subjects:
Online Access:https://www.cambridge.org/core/product/identifier/S0022143023000059/type/journal_article
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author Owen King
Sajid Ghuffar
Atanu Bhattacharya
Ruzhen Yao
Tandong Yao
Tobias Bolch
author_facet Owen King
Sajid Ghuffar
Atanu Bhattacharya
Ruzhen Yao
Tandong Yao
Tobias Bolch
author_sort Owen King
collection DOAJ
description Despite their extreme elevation, glaciers on the Tibetan Plateau are losing mass in response to atmospheric warming, the pattern of which purportedly reflects regional contrasts in climate. Here we examine the evolution of glaciers along ~500 km of the Tanggula Shan, Central-Eastern Tibetan Plateau. Using remotely sensed datasets, we quantified changes in glacier mass, area and surface velocity, and compared these results to time series of meteorological observations, in order to disentangle drivers of glacier mass loss since the 1960s. Glacier mass loss has increased (from −0.21 ± 0.12 m w.e. a−1 in 1960s–2000s, to −0.52 ± 0.18 m w.e. a−1 in 2000s–2015/18) in association with pervasive positive temperature anomalies (up to 1.85°C), which are pronounced at the end of the now lengthened ablation season. However, glacier mass budget perturbations do not mirror the magnitude of temperature anomalies in sub-regions, thus additional factors have heightened glacier recession. We show how proglacial lake expansion and glacier surging have compounded glacier recession over decadal/multi-decadal time periods, and exert similar influence on glacier mass budgets as temperature changes. Our results demonstrate the importance of ice loss mechanisms not often incorporated into broad-scale glacier projections, which need to be better considered to refine future glacier runoff estimates.
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spelling doaj.art-00c429642bb24e3db248bf7be22312312023-10-24T09:48:09ZengCambridge University PressJournal of Glaciology0022-14301727-56522023-10-01691149116610.1017/jog.2023.5Glaciological and climatological drivers of heterogeneous glacier mass loss in the Tanggula Shan (Central-Eastern Tibetan Plateau), since the 1960sOwen King0Sajid Ghuffar1Atanu Bhattacharya2https://orcid.org/0000-0001-7449-3897Ruzhen Yao3Tandong Yao4Tobias Bolch5https://orcid.org/0000-0002-8201-5059Department of Geography and Sustainable Development, University of St Andrews, St Andrews, Scotland, UKDepartment of Space Science, Institute of Space Technology, Islamabad, PakistanDepartment of Earth Sciences & Remote Sensing, JIS University, Kolkata, IndiaInstitute of Aerospace Information, Chinese Academy of Sciences, Beijing, ChinaInstitute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, ChinaDepartment of Geography and Sustainable Development, University of St Andrews, St Andrews, Scotland, UK Institute of Geodesy, Graz University of Technology, Graz, AustriaDespite their extreme elevation, glaciers on the Tibetan Plateau are losing mass in response to atmospheric warming, the pattern of which purportedly reflects regional contrasts in climate. Here we examine the evolution of glaciers along ~500 km of the Tanggula Shan, Central-Eastern Tibetan Plateau. Using remotely sensed datasets, we quantified changes in glacier mass, area and surface velocity, and compared these results to time series of meteorological observations, in order to disentangle drivers of glacier mass loss since the 1960s. Glacier mass loss has increased (from −0.21 ± 0.12 m w.e. a−1 in 1960s–2000s, to −0.52 ± 0.18 m w.e. a−1 in 2000s–2015/18) in association with pervasive positive temperature anomalies (up to 1.85°C), which are pronounced at the end of the now lengthened ablation season. However, glacier mass budget perturbations do not mirror the magnitude of temperature anomalies in sub-regions, thus additional factors have heightened glacier recession. We show how proglacial lake expansion and glacier surging have compounded glacier recession over decadal/multi-decadal time periods, and exert similar influence on glacier mass budgets as temperature changes. Our results demonstrate the importance of ice loss mechanisms not often incorporated into broad-scale glacier projections, which need to be better considered to refine future glacier runoff estimates.https://www.cambridge.org/core/product/identifier/S0022143023000059/type/journal_articleCorona KH-4glacial lakeglacier mass balancesurge-type glacierTibetan Plateau
spellingShingle Owen King
Sajid Ghuffar
Atanu Bhattacharya
Ruzhen Yao
Tandong Yao
Tobias Bolch
Glaciological and climatological drivers of heterogeneous glacier mass loss in the Tanggula Shan (Central-Eastern Tibetan Plateau), since the 1960s
Journal of Glaciology
Corona KH-4
glacial lake
glacier mass balance
surge-type glacier
Tibetan Plateau
title Glaciological and climatological drivers of heterogeneous glacier mass loss in the Tanggula Shan (Central-Eastern Tibetan Plateau), since the 1960s
title_full Glaciological and climatological drivers of heterogeneous glacier mass loss in the Tanggula Shan (Central-Eastern Tibetan Plateau), since the 1960s
title_fullStr Glaciological and climatological drivers of heterogeneous glacier mass loss in the Tanggula Shan (Central-Eastern Tibetan Plateau), since the 1960s
title_full_unstemmed Glaciological and climatological drivers of heterogeneous glacier mass loss in the Tanggula Shan (Central-Eastern Tibetan Plateau), since the 1960s
title_short Glaciological and climatological drivers of heterogeneous glacier mass loss in the Tanggula Shan (Central-Eastern Tibetan Plateau), since the 1960s
title_sort glaciological and climatological drivers of heterogeneous glacier mass loss in the tanggula shan central eastern tibetan plateau since the 1960s
topic Corona KH-4
glacial lake
glacier mass balance
surge-type glacier
Tibetan Plateau
url https://www.cambridge.org/core/product/identifier/S0022143023000059/type/journal_article
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