Glacial Isostatic Uplift in the Tibetan Plateau and Surroundings

Abstract The Tibetan Plateau and surroundings host the largest number of modern glaciers outside the polar regions. However, the impact of (de)glaciation on present‐day geodetic measurements remains unclear. Using load deformation models, we examine the glacial isostatic uplift in response to (de)gl...

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Main Authors: Shaozhuo Liu, Sigurjón Jónsson
Format: Article
Language:English
Published: Wiley 2025-07-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1029/2025GL114899
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author Shaozhuo Liu
Sigurjón Jónsson
author_facet Shaozhuo Liu
Sigurjón Jónsson
author_sort Shaozhuo Liu
collection DOAJ
description Abstract The Tibetan Plateau and surroundings host the largest number of modern glaciers outside the polar regions. However, the impact of (de)glaciation on present‐day geodetic measurements remains unclear. Using load deformation models, we examine the glacial isostatic uplift in response to (de)glaciation during the last glacial period and since the Little Ice Age. We find that the current glacial isostatic uplift locally exceeds 2.0 mm/yr near some glaciers in the Himalayas, Nyainqentanglha, Pamir, and Tien Shan. In the Nyainqentanglha, this glacial isostatic uplift could otherwise be misinterpreted as tectonic uplift associated with fictitious structures near the Jiali fault, a strike‐slip fault slipping at 2–5 mm/yr. In the Himalayas, the glacial isostatic uplift may contribute to 10%–40% of the observed 5–6 mm/yr geodetic uplift. In the Tien Shan, this ratio is 0%–50%. Therefore, glacial isostatic uplift must be considered when interpreting geodetic measurements in the Tibetan Plateau and surroundings.
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spelling doaj-art-2306bc25230b46dba96a5f6ece8ca31d2025-07-26T08:35:56ZengWileyGeophysical Research Letters0094-82761944-80072025-07-015213n/an/a10.1029/2025GL114899Glacial Isostatic Uplift in the Tibetan Plateau and SurroundingsShaozhuo Liu0Sigurjón Jónsson1Physical Science and Engineering Division King Abdullah University of Science and Technology Thuwal Saudi ArabiaPhysical Science and Engineering Division King Abdullah University of Science and Technology Thuwal Saudi ArabiaAbstract The Tibetan Plateau and surroundings host the largest number of modern glaciers outside the polar regions. However, the impact of (de)glaciation on present‐day geodetic measurements remains unclear. Using load deformation models, we examine the glacial isostatic uplift in response to (de)glaciation during the last glacial period and since the Little Ice Age. We find that the current glacial isostatic uplift locally exceeds 2.0 mm/yr near some glaciers in the Himalayas, Nyainqentanglha, Pamir, and Tien Shan. In the Nyainqentanglha, this glacial isostatic uplift could otherwise be misinterpreted as tectonic uplift associated with fictitious structures near the Jiali fault, a strike‐slip fault slipping at 2–5 mm/yr. In the Himalayas, the glacial isostatic uplift may contribute to 10%–40% of the observed 5–6 mm/yr geodetic uplift. In the Tien Shan, this ratio is 0%–50%. Therefore, glacial isostatic uplift must be considered when interpreting geodetic measurements in the Tibetan Plateau and surroundings.https://doi.org/10.1029/2025GL114899Tibetan Plateauvertical deformationglacial isostatic upliftgeodetic measurementsclimate change
spellingShingle Shaozhuo Liu
Sigurjón Jónsson
Glacial Isostatic Uplift in the Tibetan Plateau and Surroundings
Geophysical Research Letters
Tibetan Plateau
vertical deformation
glacial isostatic uplift
geodetic measurements
climate change
title Glacial Isostatic Uplift in the Tibetan Plateau and Surroundings
title_full Glacial Isostatic Uplift in the Tibetan Plateau and Surroundings
title_fullStr Glacial Isostatic Uplift in the Tibetan Plateau and Surroundings
title_full_unstemmed Glacial Isostatic Uplift in the Tibetan Plateau and Surroundings
title_short Glacial Isostatic Uplift in the Tibetan Plateau and Surroundings
title_sort glacial isostatic uplift in the tibetan plateau and surroundings
topic Tibetan Plateau
vertical deformation
glacial isostatic uplift
geodetic measurements
climate change
url https://doi.org/10.1029/2025GL114899
work_keys_str_mv AT shaozhuoliu glacialisostaticupliftinthetibetanplateauandsurroundings
AT sigurjonjonsson glacialisostaticupliftinthetibetanplateauandsurroundings