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1988 - 2018年印度锡金中型冰川的前沿变化:喜马拉雅山脉冰川 - 气候综合研究的见解

Frontal changes in medium-sized glaciers in Sikkim, India during 1988-2018: Insights for glacier-climate synthesis over the Himalaya.

作者信息

Kumar Parvendra, Sharma Milap Chand

机构信息

Department of General & Applied Geography, Dr. Harisingh Gour Vishwavidyalaya (A Central University), Sagar, Madhya Pradesh 470003, India.

Centre for the Study of Regional Development, Jawaharlal Nehru University, New Delhi 110067, India.

出版信息

iScience. 2023 Aug 30;26(10):107789. doi: 10.1016/j.isci.2023.107789. eCollection 2023 Oct 20.

Abstract

The study assesses terminus retreat of medium-sized glaciers (1988-2018) using geospatial dataset and field study in Sikkim which is under the direct influence of the Indian SW monsoon. It also explores the causes of intra-regional and inter-regional diverse patterns of glacier retreat under the purview of topographical and climatic factors to develop a glacier-climate synthesis over the region. Glaciers have retreated in a range from 63.9 to 3.9 m yr and lost a total area of ∼2.53% (0.08% yr) in the study area. The intra-regional heterogeneity in glaciers retreat seems to be caused by topographical factors in the study area. A comparison of glacier retreats with other parts of the Himalayas reveals a declining gradient from the northwest to the eastern Himalayas, broadly. This inter-regional disparity in the retreat rate seems to be caused by existing climatic regimes over different parts of the Himalayas. The results help to comprehend the glacier-climate synthesis over the Himalayan region.

摘要

该研究利用地理空间数据集并通过实地考察,评估了锡金邦受印度西南季风直接影响的中型冰川(1988 - 2018年)的末端退缩情况。研究还探讨了在地形和气候因素影响下,区域内和区域间冰川退缩模式多样的原因,以建立该地区的冰川 - 气候综合模型。在研究区域内,冰川退缩速度在63.9至3.9米/年之间,总面积减少了约2.53%(0.08%/年)。研究区域内冰川退缩的区域异质性似乎是由地形因素造成的。与喜马拉雅山脉其他地区的冰川退缩情况相比,总体上呈现出从西北到东喜马拉雅逐渐下降的梯度。这种退缩速率的区域差异似乎是由喜马拉雅山脉不同地区现有的气候状况导致的。研究结果有助于理解喜马拉雅地区的冰川 - 气候综合模型。

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