Evaluating the contribution of avalanching to the mass balance of Himalayan glaciers

Avalanching is a prominent source of accumulation on glaciers that have high and steep valley-walls surrounding their accumulation zones. These glaciers are typically characterised by an extensive supraglacial debris cover and a low accumulation area ratio. Despite an abundance of such glaciers in t...

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Main Authors: Sourav Laha, Reshama Kumari, Sunil Singh, Aditya Mishra, Tushar Sharma, Argha Banerjee, Harish Chandra Nainwal, R. Shankar
Format: Article
Language:English
Published: Cambridge University Press 2017-07-01
Series:Annals of Glaciology
Subjects:
Online Access:https://www.cambridge.org/core/product/identifier/S0260305517000271/type/journal_article
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author Sourav Laha
Reshama Kumari
Sunil Singh
Aditya Mishra
Tushar Sharma
Argha Banerjee
Harish Chandra Nainwal
R. Shankar
author_facet Sourav Laha
Reshama Kumari
Sunil Singh
Aditya Mishra
Tushar Sharma
Argha Banerjee
Harish Chandra Nainwal
R. Shankar
author_sort Sourav Laha
collection DOAJ
description Avalanching is a prominent source of accumulation on glaciers that have high and steep valley-walls surrounding their accumulation zones. These glaciers are typically characterised by an extensive supraglacial debris cover and a low accumulation area ratio. Despite an abundance of such glaciers in the rugged landscapes of the High Himalaya, attempts to quantify the net avalanche contribution to mass balance and its long-term variation are almost missing. We first discuss diagnostic criteria to identify strongly avalanche-fed glaciers. Second, we develop an approximate method to quantify the magnitude of the avalanche accumulation exploiting its expected control on the dynamics of these glaciers. The procedure is based on a simplified flowline model description of the glacier concerned and utilises the known glaciological mass-balance, velocity and surface-elevation profiles of the glacier. We apply the method to three Himalayan glaciers and show that the data on the recent dynamics of these glaciers are consistent with a dominant contribution of avalanches to the total accumulation. As a control experiment, we also simulate another Himalayan glacier where no significant avalanche contribution is expected, and reproduce the recent changes in that glacier without any additional avalanche contribution.
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spelling doaj.art-9c1c317358c54c9ba4fb5d557a77deed2023-03-09T12:27:29ZengCambridge University PressAnnals of Glaciology0260-30551727-56442017-07-015811011810.1017/aog.2017.27Evaluating the contribution of avalanching to the mass balance of Himalayan glaciersSourav Laha0Reshama Kumari1Sunil Singh2Aditya Mishra3Tushar Sharma4Argha Banerjee5Harish Chandra Nainwal6R. Shankar7Earth and Climate Science, Indian Institute of Science Education and Research, Pune, India E-mail:Earth and Climate Science, Indian Institute of Science Education and Research, Pune, India E-mail:Department of Geology, HNB Garhwal University, Srinagar Garhwal, Uttarakhand 246174, IndiaDepartment of Geology, HNB Garhwal University, Srinagar Garhwal, Uttarakhand 246174, IndiaDepartment of Geology, HNB Garhwal University, Srinagar Garhwal, Uttarakhand 246174, IndiaEarth and Climate Science, Indian Institute of Science Education and Research, Pune, India E-mail:Department of Geology, HNB Garhwal University, Srinagar Garhwal, Uttarakhand 246174, IndiaThe Institute of Mathematical Sciences, Chennai 600113, IndiaAvalanching is a prominent source of accumulation on glaciers that have high and steep valley-walls surrounding their accumulation zones. These glaciers are typically characterised by an extensive supraglacial debris cover and a low accumulation area ratio. Despite an abundance of such glaciers in the rugged landscapes of the High Himalaya, attempts to quantify the net avalanche contribution to mass balance and its long-term variation are almost missing. We first discuss diagnostic criteria to identify strongly avalanche-fed glaciers. Second, we develop an approximate method to quantify the magnitude of the avalanche accumulation exploiting its expected control on the dynamics of these glaciers. The procedure is based on a simplified flowline model description of the glacier concerned and utilises the known glaciological mass-balance, velocity and surface-elevation profiles of the glacier. We apply the method to three Himalayan glaciers and show that the data on the recent dynamics of these glaciers are consistent with a dominant contribution of avalanches to the total accumulation. As a control experiment, we also simulate another Himalayan glacier where no significant avalanche contribution is expected, and reproduce the recent changes in that glacier without any additional avalanche contribution.https://www.cambridge.org/core/product/identifier/S0260305517000271/type/journal_articleAvalanchesdebris-covered glaciersglacier mass balanceglacier modelling
spellingShingle Sourav Laha
Reshama Kumari
Sunil Singh
Aditya Mishra
Tushar Sharma
Argha Banerjee
Harish Chandra Nainwal
R. Shankar
Evaluating the contribution of avalanching to the mass balance of Himalayan glaciers
Annals of Glaciology
Avalanches
debris-covered glaciers
glacier mass balance
glacier modelling
title Evaluating the contribution of avalanching to the mass balance of Himalayan glaciers
title_full Evaluating the contribution of avalanching to the mass balance of Himalayan glaciers
title_fullStr Evaluating the contribution of avalanching to the mass balance of Himalayan glaciers
title_full_unstemmed Evaluating the contribution of avalanching to the mass balance of Himalayan glaciers
title_short Evaluating the contribution of avalanching to the mass balance of Himalayan glaciers
title_sort evaluating the contribution of avalanching to the mass balance of himalayan glaciers
topic Avalanches
debris-covered glaciers
glacier mass balance
glacier modelling
url https://www.cambridge.org/core/product/identifier/S0260305517000271/type/journal_article
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