Significant changes of area, length and terminus of Sikkim Himalayan glaciers within the Kanchenjunga national park from 1990 - 2022

Soumik Saha , Biswajit Bera , Sumana Bhattacharjee , Nairita Sengupta , Mridul Barman
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Abstract

In this study, we have investigated four glaciers, namely Zemu, Talung, Alukthang and Rathong within Kanchenjunga national park. This study evaluates physical and morphometric parameters (area, length, perimeter, area of accumulation zone, ablation zone length, snout position, thickness and specific mass balance) of multiple glaciers and to ascertain the poorly understood glaciers of western Sikkim region under Kanchenjunga national park. The principal objective of this research is to find out the changes of glacial mass and other physical parameters of the selected glaciers using multi sources digital elevation model data.Various techniques of statistics, including Mann-Kendall and Sen’s slope tests have been applied at different confidence interval. We have identified that climate change is responsible for the alterations of the physical characteristics of the glaciers. Result shows that during the study period, Zemu glacier has faced highest amount of deglaciation in terms of area (20.79 sq.km) along with maximum 30 m elevation reduction, 24 m increase of snout elevation and 200 m retreat of terminus. Furthermore, it is observed that terminus of the each selected glaciers retreated during the study period. Rathong experienced maximum retreat rate, approximately 550 m, and is accompanied by a notable 163% increase in the ablation zone. Alukthang and Talung reduced their areas 0.56 and 4.06 sq.km respectively, along with 2.75 m and 9.10 m thickness respectively. Maximum 36.39 m/y-1 flow rate has been observed over Zemu glacier. The flow rate of Talung, Rathong and Alukthang glacier is 26.4 m/y-1, 34.1 m/y-1, and 23.7 m/y-1 respectively.

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1990-2022 年间坎钦贡嘎国家公园内锡金喜马拉雅冰川面积、长度和终点的显著变化
在这项研究中,我们调查了康钦宗迦国家公园内的四座冰川,即泽木冰川、塔隆冰川、阿鲁克唐冰川和拉通冰川。这项研究评估了多条冰川的物理和形态参数(面积、长度、周长、积聚区面积、消融区长度、吻部位置、厚度和特定质量平衡),并确定了坎钦贡嘎国家公园内西锡金地区不为人知的冰川。这项研究的主要目的是利用多种来源的数字高程模型数据,找出选定冰川的冰川质量和其他物理参数的变化。我们发现气候变化是冰川物理特征发生变化的原因。研究结果表明,在研究期间,泽木冰川面临的冰川退化面积最大(20.79 平方公里),海拔降低了 30 米,鼻端海拔升高了 24 米,终点后退了 200 米。此外,在研究期间,每个选定冰川的末端都出现了后退。拉通冰川的后退速度最大,约为 550 米,同时消融区明显扩大了 163%。阿鲁塘和塔隆的面积分别减少了 0.56 和 4.06 平方公里,厚度分别减少了 2.75 米和 9.10 米。泽木冰川的最大流速为 36.39 米/年-1。塔隆、拉通和阿鲁克唐冰川的流速分别为 26.4 米/年-1、34.1 米/年-1 和 23.7 米/年-1。
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