No significant mass loss in the glaciers of Astore Basin (North-Western Himalaya), between 1999 and 2016

Although glaciers in High Mountain Asia produce an enormous amount of water used by downstream populations, they remain poorly observed in the field. This study presents a geodetic mass balance of the glaciers in the Astore Basin (with differential GPS (dGPS) measurements on Harcho glacier) between...

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Main Authors: SHER MUHAMMAD, LIDE TIAN, MARCUS NÜSSER
Format: Article
Language:English
Published: Cambridge University Press 2019-04-01
Series:Journal of Glaciology
Subjects:
Online Access:https://www.cambridge.org/core/product/identifier/S0022143019000054/type/journal_article
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author SHER MUHAMMAD
LIDE TIAN
MARCUS NÜSSER
author_facet SHER MUHAMMAD
LIDE TIAN
MARCUS NÜSSER
author_sort SHER MUHAMMAD
collection DOAJ
description Although glaciers in High Mountain Asia produce an enormous amount of water used by downstream populations, they remain poorly observed in the field. This study presents a geodetic mass balance of the glaciers in the Astore Basin (with differential GPS (dGPS) measurements on Harcho glacier) between 1999 and 2016. Changes near the terminus of Harcho glacier (below 3800 m a.s.l.) featured heterogeneous surface elevation changes, whereas the middle section shows the most negative changes. The surface elevation changes were positive above 4200 m a.s.l. The average annual mass balance was −0.08 ± 0.07 m w.e. a−1 derived from a dGPS and DEM comparison whereas Advanced Spaceborne Thermal Emission and Reflection Radiometer DEM-based results show a slightly positive, that is 0.03 ± 0.24 m w.e. a−1 in the same period. In contrast, the terminus indicates a substantial retreat of ~368 m (4.5 m a−1) between 1934 and 2016. The average mass balance of 19 glaciers (>2 km2) covering ~60% of the total glaciers in the Basin exhibit no net mass loss in the period of 2000−2016 and follow a pattern similar to adjacent Karakoram glaciers.
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spelling doaj.art-dfe2f968edf74738ba3bb5f12bde4d6c2023-03-09T12:40:44ZengCambridge University PressJournal of Glaciology0022-14301727-56522019-04-016527027810.1017/jog.2019.5No significant mass loss in the glaciers of Astore Basin (North-Western Himalaya), between 1999 and 2016SHER MUHAMMAD0https://orcid.org/0000-0001-7315-6450LIDE TIAN1MARCUS NÜSSER2Institute of International Rivers and Eco-security, Yunnan University, 650500 Kunming, China Yunnan Key Laboratory of International Rivers and Transboundary Eco–security, Kunming 650091, China Key Laboratory of Tibetan Environmental Change and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China International Center for Integrated Mountain Development (ICIMOD), Kathmandu, NepalInstitute of International Rivers and Eco-security, Yunnan University, 650500 Kunming, China Yunnan Key Laboratory of International Rivers and Transboundary Eco–security, Kunming 650091, China Key Laboratory of Tibetan Environmental Change and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China CAS Center of Excellence in Tibetan Plateau Earth Sciences, Beijing 100101, ChinaDepartment of Geography, South Asia Institute, Heidelberg University, GermanyAlthough glaciers in High Mountain Asia produce an enormous amount of water used by downstream populations, they remain poorly observed in the field. This study presents a geodetic mass balance of the glaciers in the Astore Basin (with differential GPS (dGPS) measurements on Harcho glacier) between 1999 and 2016. Changes near the terminus of Harcho glacier (below 3800 m a.s.l.) featured heterogeneous surface elevation changes, whereas the middle section shows the most negative changes. The surface elevation changes were positive above 4200 m a.s.l. The average annual mass balance was −0.08 ± 0.07 m w.e. a−1 derived from a dGPS and DEM comparison whereas Advanced Spaceborne Thermal Emission and Reflection Radiometer DEM-based results show a slightly positive, that is 0.03 ± 0.24 m w.e. a−1 in the same period. In contrast, the terminus indicates a substantial retreat of ~368 m (4.5 m a−1) between 1934 and 2016. The average mass balance of 19 glaciers (>2 km2) covering ~60% of the total glaciers in the Basin exhibit no net mass loss in the period of 2000−2016 and follow a pattern similar to adjacent Karakoram glaciers.https://www.cambridge.org/core/product/identifier/S0022143019000054/type/journal_articleglacier mass balanceglacier mappingdGPSremote sensing
spellingShingle SHER MUHAMMAD
LIDE TIAN
MARCUS NÜSSER
No significant mass loss in the glaciers of Astore Basin (North-Western Himalaya), between 1999 and 2016
Journal of Glaciology
glacier mass balance
glacier mapping
dGPS
remote sensing
title No significant mass loss in the glaciers of Astore Basin (North-Western Himalaya), between 1999 and 2016
title_full No significant mass loss in the glaciers of Astore Basin (North-Western Himalaya), between 1999 and 2016
title_fullStr No significant mass loss in the glaciers of Astore Basin (North-Western Himalaya), between 1999 and 2016
title_full_unstemmed No significant mass loss in the glaciers of Astore Basin (North-Western Himalaya), between 1999 and 2016
title_short No significant mass loss in the glaciers of Astore Basin (North-Western Himalaya), between 1999 and 2016
title_sort no significant mass loss in the glaciers of astore basin north western himalaya between 1999 and 2016
topic glacier mass balance
glacier mapping
dGPS
remote sensing
url https://www.cambridge.org/core/product/identifier/S0022143019000054/type/journal_article
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AT lidetian nosignificantmasslossintheglaciersofastorebasinnorthwesternhimalayabetween1999and2016
AT marcusnusser nosignificantmasslossintheglaciersofastorebasinnorthwesternhimalayabetween1999and2016