Projection of glacier changes over the Laohugou Glacier No. 12, Northeast Tibetan Plateau, China from 2020 to 2100

Study region: Laohugou Glacier No. 12 in the Qilian Mountains, northeast Tibetan Plateau. Study focus: Alpine glacier meltwater from the Qilian Mountains (QMs), northeast Tibetan Plateau, is the main source of water for the surrounding arid zones. Accurately reconstructing long-term mountain glacier...

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Main Authors: Mengyuan Liu, Baojuan Huai, Lei Wang, Yuzhe Wang, Hongmin An, Jizu Chen, Wentao Du, Xiang Qin, Weijun Sun
Format: Article
Language:English
Published: Elsevier 2025-02-01
Series:Journal of Hydrology: Regional Studies
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Online Access:http://www.sciencedirect.com/science/article/pii/S2214581824004385
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author Mengyuan Liu
Baojuan Huai
Lei Wang
Yuzhe Wang
Hongmin An
Jizu Chen
Wentao Du
Xiang Qin
Weijun Sun
author_facet Mengyuan Liu
Baojuan Huai
Lei Wang
Yuzhe Wang
Hongmin An
Jizu Chen
Wentao Du
Xiang Qin
Weijun Sun
author_sort Mengyuan Liu
collection DOAJ
description Study region: Laohugou Glacier No. 12 in the Qilian Mountains, northeast Tibetan Plateau. Study focus: Alpine glacier meltwater from the Qilian Mountains (QMs), northeast Tibetan Plateau, is the main source of water for the surrounding arid zones. Accurately reconstructing long-term mountain glacier mass balance (MB) and projecting glacier changes under climate warming are pivotal in cryospheric scientific research. In this study, Laohugou Glacier No. 12 (LHG12), in the western QMs, was selected as a study area. Based on the Coupled Model Intercomparison Project (CMIP6) models, the degree-day and glacier retreat models were used to predict the glacier changes under three scenarios for 2020–2100. New hydrological insights for the region: From 2020–2100, the annual mass loss of LHG12 simulated using CanESM5 and EC-Earth3 which perform best increased compared to the measured data in the historical period (2010–2014) (i.e., annual MB of −0.26 m w.e) by a factor of 1.04 and 1.73 under SSP1–2.6, 4.62 and 4.88 under SSP3–7.0, and 6.23 and 7.15 times under SSP5–8.5. By 2100, the ice volume and area of LHG12 simulated using CanESM5 and EC-Earth3 reduced to 0.03×109 (1.6 %) and 0.01×109 (0.4 %) m3, 1.87 and 0.75 km2 under SSP5–8.5, respectively.
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spelling doaj-art-711f0ce6448f4d9ba92bf2130de7a6af2025-01-22T05:41:58ZengElsevierJournal of Hydrology: Regional Studies2214-58182025-02-0157102089Projection of glacier changes over the Laohugou Glacier No. 12, Northeast Tibetan Plateau, China from 2020 to 2100Mengyuan Liu0Baojuan Huai1Lei Wang2Yuzhe Wang3Hongmin An4Jizu Chen5Wentao Du6Xiang Qin7Weijun Sun8College of Geography and Environment, Shandong Normal University, Jinan 250014, ChinaCollege of Geography and Environment, Shandong Normal University, Jinan 250014, China; Corresponding authors.College of Geography and Environment, Shandong Normal University, Jinan 250014, ChinaCollege of Geography and Environment, Shandong Normal University, Jinan 250014, ChinaCollege of Geography and Environment, Shandong Normal University, Jinan 250014, ChinaQilian Shan Station of Glaciology and Eco-environment, Key Laboratory of Cryospheric Science and Frozen Soil Engineering, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, ChinaQilian Shan Station of Glaciology and Eco-environment, Key Laboratory of Cryospheric Science and Frozen Soil Engineering, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, ChinaQilian Shan Station of Glaciology and Eco-environment, Key Laboratory of Cryospheric Science and Frozen Soil Engineering, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, ChinaCollege of Geography and Environment, Shandong Normal University, Jinan 250014, China; Corresponding authors.Study region: Laohugou Glacier No. 12 in the Qilian Mountains, northeast Tibetan Plateau. Study focus: Alpine glacier meltwater from the Qilian Mountains (QMs), northeast Tibetan Plateau, is the main source of water for the surrounding arid zones. Accurately reconstructing long-term mountain glacier mass balance (MB) and projecting glacier changes under climate warming are pivotal in cryospheric scientific research. In this study, Laohugou Glacier No. 12 (LHG12), in the western QMs, was selected as a study area. Based on the Coupled Model Intercomparison Project (CMIP6) models, the degree-day and glacier retreat models were used to predict the glacier changes under three scenarios for 2020–2100. New hydrological insights for the region: From 2020–2100, the annual mass loss of LHG12 simulated using CanESM5 and EC-Earth3 which perform best increased compared to the measured data in the historical period (2010–2014) (i.e., annual MB of −0.26 m w.e) by a factor of 1.04 and 1.73 under SSP1–2.6, 4.62 and 4.88 under SSP3–7.0, and 6.23 and 7.15 times under SSP5–8.5. By 2100, the ice volume and area of LHG12 simulated using CanESM5 and EC-Earth3 reduced to 0.03×109 (1.6 %) and 0.01×109 (0.4 %) m3, 1.87 and 0.75 km2 under SSP5–8.5, respectively.http://www.sciencedirect.com/science/article/pii/S2214581824004385Climate changeMass balanceCMIP6Laohugou Glacier No.12Glacier model
spellingShingle Mengyuan Liu
Baojuan Huai
Lei Wang
Yuzhe Wang
Hongmin An
Jizu Chen
Wentao Du
Xiang Qin
Weijun Sun
Projection of glacier changes over the Laohugou Glacier No. 12, Northeast Tibetan Plateau, China from 2020 to 2100
Journal of Hydrology: Regional Studies
Climate change
Mass balance
CMIP6
Laohugou Glacier No.12
Glacier model
title Projection of glacier changes over the Laohugou Glacier No. 12, Northeast Tibetan Plateau, China from 2020 to 2100
title_full Projection of glacier changes over the Laohugou Glacier No. 12, Northeast Tibetan Plateau, China from 2020 to 2100
title_fullStr Projection of glacier changes over the Laohugou Glacier No. 12, Northeast Tibetan Plateau, China from 2020 to 2100
title_full_unstemmed Projection of glacier changes over the Laohugou Glacier No. 12, Northeast Tibetan Plateau, China from 2020 to 2100
title_short Projection of glacier changes over the Laohugou Glacier No. 12, Northeast Tibetan Plateau, China from 2020 to 2100
title_sort projection of glacier changes over the laohugou glacier no 12 northeast tibetan plateau china from 2020 to 2100
topic Climate change
Mass balance
CMIP6
Laohugou Glacier No.12
Glacier model
url http://www.sciencedirect.com/science/article/pii/S2214581824004385
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