R
Rupendra Singh
Researcher at Jawaharlal Nehru University
Publications - 12
Citations - 116
Rupendra Singh is an academic researcher from Jawaharlal Nehru University. The author has contributed to research in topics: Glacier & Glacial period. The author has an hindex of 6, co-authored 9 publications receiving 63 citations. Previous affiliations of Rupendra Singh include Sharda University.
Papers
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Lake Inventory and Evolution of Glacial Lakes in the Nubra-Shyok Basin of Karakoram Range
TL;DR: In this article, the authors investigate the growth and changes in moraine and bed rock dammed glacier lakes of the Nubra and Shyok basin, Karakoram Range using multi-temporal satellite images.
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Causes and geomorphological effects of large debris flows in the lower valley areas of the Meru and Gangotri glaciers, Bhagirathi basin, Garhwal Himalaya (India)
TL;DR: In this article, the authors investigated the debris flow occurred in July 2017 at the terminal moraine of the Meru glacier, Bhagirathi basin, Garhwal Himalaya.
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Flood hazard assessment of August 20, 2016 floods in Satna District, Madhya Pradesh, India
TL;DR: In this paper, a flood hazard index (FHI) using linear combination of only two parameters (tasseled cap wetness index and modified normalised difference water index (MNDWI) was proposed.
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Climate forcing and the initiation of glacier advance during MIS-2 in the North Sikkim Himalaya, India
TL;DR: In this article, the authors investigated the relics of the most extensive glacier advances and their retreat in the transitional climatic zone of the Chopta valley, northern Sikkim Himalaya with an aim to understand the forcing factors.
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Glacial Geomorphology and Landscape Evolution of the Thangu Valley, North Sikkim Himalaya, India
Jyotsna Dubey,Sheikh Nawaz Ali,Anupam Sharma,P. Morthekai,Rupendra Singh,R. K. Sharma,Pratima Pandey,Biswajeet Thakur,Vaibhava Srivastava +8 more
TL;DR: In this paper, the authors describe detailed glacial geomorphology of Lashar and Chopta valleys as the area is strongly modified by the erosional and depositional imprints of late Pleistocene glaciations (MIS 2) and also provide significant insights about the evolution of pro and paraglacial landscapes.