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

ABSTRACT 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 glac...

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Published in:Annals of Glaciology
Main Authors: Laha, Sourav, Kumari, Reshama, Singh, Sunil, Mishra, Aditya, Sharma, Tushar, Banerjee, Argha, Nainwal, Harish Chandra, Shankar, R.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2017
Subjects:
Online Access:http://dx.doi.org/10.1017/aog.2017.27
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0260305517000271
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spelling crcambridgeupr:10.1017/aog.2017.27 2024-06-23T07:45:36+00:00 Evaluating the contribution of avalanching to the mass balance of Himalayan glaciers Laha, Sourav Kumari, Reshama Singh, Sunil Mishra, Aditya Sharma, Tushar Banerjee, Argha Nainwal, Harish Chandra Shankar, R. 2017 http://dx.doi.org/10.1017/aog.2017.27 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0260305517000271 en eng Cambridge University Press (CUP) Annals of Glaciology volume 58, issue 75pt2, page 110-118 ISSN 0260-3055 1727-5644 journal-article 2017 crcambridgeupr https://doi.org/10.1017/aog.2017.27 2024-06-12T04:04:00Z ABSTRACT 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. Article in Journal/Newspaper Annals of Glaciology Cambridge University Press Annals of Glaciology 58 75pt2 110 118
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description ABSTRACT 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.
format Article in Journal/Newspaper
author Laha, Sourav
Kumari, Reshama
Singh, Sunil
Mishra, Aditya
Sharma, Tushar
Banerjee, Argha
Nainwal, Harish Chandra
Shankar, R.
spellingShingle Laha, Sourav
Kumari, Reshama
Singh, Sunil
Mishra, Aditya
Sharma, Tushar
Banerjee, Argha
Nainwal, Harish Chandra
Shankar, R.
Evaluating the contribution of avalanching to the mass balance of Himalayan glaciers
author_facet Laha, Sourav
Kumari, Reshama
Singh, Sunil
Mishra, Aditya
Sharma, Tushar
Banerjee, Argha
Nainwal, Harish Chandra
Shankar, R.
author_sort Laha, Sourav
title 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_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_sort evaluating the contribution of avalanching to the mass balance of himalayan glaciers
publisher Cambridge University Press (CUP)
publishDate 2017
url http://dx.doi.org/10.1017/aog.2017.27
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0260305517000271
genre Annals of Glaciology
genre_facet Annals of Glaciology
op_source Annals of Glaciology
volume 58, issue 75pt2, page 110-118
ISSN 0260-3055 1727-5644
op_doi https://doi.org/10.1017/aog.2017.27
container_title Annals of Glaciology
container_volume 58
container_issue 75pt2
container_start_page 110
op_container_end_page 118
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