Understanding the point mass balance and surface ice velocity for the debris-covered glacier, Panchi II, western Himalaya (India)

Debris-covered glaciers with complex morphological features, including ice cliffs and supraglacial lakes, remain relatively understudied in the Himalaya. Panchi II Glacier, located in the Bhaga Basin of the western Himalaya, exemplifies such complex debris-covered glacier. We conducted assessments o...

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Main Authors: Sarvagya Vatsal, Mohd Farooq Azam, Anshuman Bhardwaj, Arindan Mandal, Raaj Ramsankaran, Mohd Soheb, Saumya G. Kutty, Chetan Singh, Somdutta Mishra, Alagappan Ramanathan, Ishmohan Bahuguna, Purvee Joshi, N. Janardhana Raju
Format: Article
Language:English
Published: Elsevier 2025-12-01
Series:Results in Earth Sciences
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Online Access:http://www.sciencedirect.com/science/article/pii/S2211714824000451
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author Sarvagya Vatsal
Mohd Farooq Azam
Anshuman Bhardwaj
Arindan Mandal
Raaj Ramsankaran
Mohd Soheb
Saumya G. Kutty
Chetan Singh
Somdutta Mishra
Alagappan Ramanathan
Ishmohan Bahuguna
Purvee Joshi
N. Janardhana Raju
author_facet Sarvagya Vatsal
Mohd Farooq Azam
Anshuman Bhardwaj
Arindan Mandal
Raaj Ramsankaran
Mohd Soheb
Saumya G. Kutty
Chetan Singh
Somdutta Mishra
Alagappan Ramanathan
Ishmohan Bahuguna
Purvee Joshi
N. Janardhana Raju
author_sort Sarvagya Vatsal
collection DOAJ
description Debris-covered glaciers with complex morphological features, including ice cliffs and supraglacial lakes, remain relatively understudied in the Himalaya. Panchi II Glacier, located in the Bhaga Basin of the western Himalaya, exemplifies such complex debris-covered glacier. We conducted assessments of both the point mass balances and the surface ice velocity of the Panchi II Glacier. We measured the debris thickness at various elevation zones and observed non-uniformity in the debris thickness across the glacier. To understand the influence of debris thickness, our methodology encompassed the direct glaciological approach for point mass balance estimation, complemented by DGPS surveying and satellite-derived datasets for surface ice velocity estimation. The point mass balance for 2017–2021 indicates that debris thickness is a key factor in regulating glacier melt. Mean surface ice velocity of the whole glacier for the year 2019/21 was 9.2 ± 1.5 m a−1. Our findings indicate that for Panchi II Glacier melting is predominantly governed by debris thickness rather than elevation. Furthermore, multivariate linear analysis reveals that elevation, debris thickness, and slope explain 91 % variability in the surface ice velocity of the glacier.
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institution Kabale University
issn 2211-7148
language English
publishDate 2025-12-01
publisher Elsevier
record_format Article
series Results in Earth Sciences
spelling doaj-art-b24b3acbb9684320a1dee58db89b95722025-01-08T04:52:26ZengElsevierResults in Earth Sciences2211-71482025-12-013100058Understanding the point mass balance and surface ice velocity for the debris-covered glacier, Panchi II, western Himalaya (India)Sarvagya Vatsal0Mohd Farooq Azam1Anshuman Bhardwaj2Arindan Mandal3Raaj Ramsankaran4Mohd Soheb5Saumya G. Kutty6Chetan Singh7Somdutta Mishra8Alagappan Ramanathan9Ishmohan Bahuguna10Purvee Joshi11N. Janardhana Raju12School of Geosciences, University of Aberdeen, King’s College, Aberdeen, United Kingdom; Department of Civil Engineering, Indian Institute of Technology Indore, Simrol, Madhya Pradesh, India; School of Environmental Sciences, Jawaharlal Nehru University, New Delhi, India; Corresponding author at: School of Geosciences, University of Aberdeen, King’s College, Aberdeen, United Kingdom.Department of Civil Engineering, Indian Institute of Technology Indore, Simrol, Madhya Pradesh, IndiaSchool of Geosciences, University of Aberdeen, King’s College, Aberdeen, United KingdomInterdisciplinary Centre for Water Research, Indian Institute of Science Bangalore, Karnataka, IndiaDepartment of Civil Engineering, Indian Institute of Technology Bombay, Maharashtra, IndiaDepartment of Geography, South Asia Institute, Heidelberg University, Heidelberg, GermanySchool of Environmental Sciences, Jawaharlal Nehru University, New Delhi, IndiaSchool of Environmental Sciences, Jawaharlal Nehru University, New Delhi, IndiaSchool of Environmental Sciences, Jawaharlal Nehru University, New Delhi, IndiaSchool of Environmental Sciences, Jawaharlal Nehru University, New Delhi, IndiaSpace Application Centre, Indian Space Research Organisation, Ahmedabad, IndiaSpace Application Centre, Indian Space Research Organisation, Ahmedabad, IndiaSchool of Environmental Sciences, Jawaharlal Nehru University, New Delhi, IndiaDebris-covered glaciers with complex morphological features, including ice cliffs and supraglacial lakes, remain relatively understudied in the Himalaya. Panchi II Glacier, located in the Bhaga Basin of the western Himalaya, exemplifies such complex debris-covered glacier. We conducted assessments of both the point mass balances and the surface ice velocity of the Panchi II Glacier. We measured the debris thickness at various elevation zones and observed non-uniformity in the debris thickness across the glacier. To understand the influence of debris thickness, our methodology encompassed the direct glaciological approach for point mass balance estimation, complemented by DGPS surveying and satellite-derived datasets for surface ice velocity estimation. The point mass balance for 2017–2021 indicates that debris thickness is a key factor in regulating glacier melt. Mean surface ice velocity of the whole glacier for the year 2019/21 was 9.2 ± 1.5 m a−1. Our findings indicate that for Panchi II Glacier melting is predominantly governed by debris thickness rather than elevation. Furthermore, multivariate linear analysis reveals that elevation, debris thickness, and slope explain 91 % variability in the surface ice velocity of the glacier.http://www.sciencedirect.com/science/article/pii/S2211714824000451Debris-covered glacierWestern HimalayaPoint mass balanceSurface ice velocity
spellingShingle Sarvagya Vatsal
Mohd Farooq Azam
Anshuman Bhardwaj
Arindan Mandal
Raaj Ramsankaran
Mohd Soheb
Saumya G. Kutty
Chetan Singh
Somdutta Mishra
Alagappan Ramanathan
Ishmohan Bahuguna
Purvee Joshi
N. Janardhana Raju
Understanding the point mass balance and surface ice velocity for the debris-covered glacier, Panchi II, western Himalaya (India)
Results in Earth Sciences
Debris-covered glacier
Western Himalaya
Point mass balance
Surface ice velocity
title Understanding the point mass balance and surface ice velocity for the debris-covered glacier, Panchi II, western Himalaya (India)
title_full Understanding the point mass balance and surface ice velocity for the debris-covered glacier, Panchi II, western Himalaya (India)
title_fullStr Understanding the point mass balance and surface ice velocity for the debris-covered glacier, Panchi II, western Himalaya (India)
title_full_unstemmed Understanding the point mass balance and surface ice velocity for the debris-covered glacier, Panchi II, western Himalaya (India)
title_short Understanding the point mass balance and surface ice velocity for the debris-covered glacier, Panchi II, western Himalaya (India)
title_sort understanding the point mass balance and surface ice velocity for the debris covered glacier panchi ii western himalaya india
topic Debris-covered glacier
Western Himalaya
Point mass balance
Surface ice velocity
url http://www.sciencedirect.com/science/article/pii/S2211714824000451
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