Assessment of recent changes (2011–2020) in glacier thickness and runoff variability in Gangotri glacier, India

Recent evidence shows a noticeable reduction in the glacier mass in the Himalaya due to increasing temperatures, and therefore the downstream water availability is becoming uncertain. This study analyse the effect of changes in the Gangotri glaciers (i.e. thickness), including Raktavaran and Chatura...

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Bibliographic Details
Published in:Hydrological sciences journal Vol. 68; no. 15; pp. 2223 - 2242
Main Authors: Singh, Japjeet, Singh, Vishal, Ojha, Chandra Shekhar Prasad, Arora, Manohar K.
Format: Journal Article
Language:English
Published: Abingdon Taylor & Francis 18-11-2023
Taylor & Francis Ltd
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Summary:Recent evidence shows a noticeable reduction in the glacier mass in the Himalaya due to increasing temperatures, and therefore the downstream water availability is becoming uncertain. This study analyse the effect of changes in the Gangotri glaciers (i.e. thickness), including Raktavaran and Chaturangi regions, on the melt runoff (2011–2020) by coupling two models: Glacier Bed Topolology (GlabTop2) and Spatial Process in Hydrology (SPHY). This study performs the two-step calibration approach utilizing the observed discharge and Moderate Resolution Imaging Spectroradiometer (MODIS) snow cover data. The R 2 values for SPHY-modelled runoff (Q) and observed Q at Bhojwasa are found comparable (~0.73 on a daily scale) and the proportions of glacier Q and snow Q in total Q are computed as 22.11% and 66.91%, respectively. In comparison to Chaturangi and Raktavaran, Gangotri glaciers experienced a higher rate of change in thickness, and a reduction of ~9.40% in the mean glacier thickness is calculated during 2011–2020.
ISSN:0262-6667
2150-3435
DOI:10.1080/02626667.2023.2258861