Volume-area scaling for debris-covered glaciers

A volume-area scaling relation is commonly used to estimate glacier volume or its future changes on a global scale. The presence of an insulating supraglacial debris cover alters the mass-balance profile of a glacier, potentially modifying the scaling relation. Here, the nature of scaling relations...

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Published in:Journal of Glaciology
Main Author: Argha Banerjee
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2020
Subjects:
Online Access:https://doi.org/10.1017/jog.2020.69
https://doaj.org/article/817de9ece0c841f398d2f34328aeab24
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spelling ftdoajarticles:oai:doaj.org/article:817de9ece0c841f398d2f34328aeab24 2023-05-15T16:57:34+02:00 Volume-area scaling for debris-covered glaciers Argha Banerjee 2020-10-01T00:00:00Z https://doi.org/10.1017/jog.2020.69 https://doaj.org/article/817de9ece0c841f398d2f34328aeab24 EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143020000696/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2020.69 0022-1430 1727-5652 https://doaj.org/article/817de9ece0c841f398d2f34328aeab24 Journal of Glaciology, Vol 66, Pp 880-886 (2020) Debris-covered glaciers mountain glaciers volume scaling methods Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2020 ftdoajarticles https://doi.org/10.1017/jog.2020.69 2023-03-12T01:30:57Z A volume-area scaling relation is commonly used to estimate glacier volume or its future changes on a global scale. The presence of an insulating supraglacial debris cover alters the mass-balance profile of a glacier, potentially modifying the scaling relation. Here, the nature of scaling relations for extensively debris-covered glaciers is investigated. Theoretical arguments suggest that the volume-area scaling exponent for these glaciers is ~7% smaller than that for clean glaciers. This is consistent with the results from flowline-model simulations of idealised glaciers, and the available data from the Himalaya. The best-fit scale factor for debris-covered Himalayan glaciers is ~60% larger compared to that for the clean ones, implying a significantly larger stored ice volume in a debris-covered glacier compared to a clean one having the same area. These results may help improve scaling-based estimates of glacier volume and future glacier changes in regions where debris-covered glaciers are abundant. Article in Journal/Newspaper Journal of Glaciology Directory of Open Access Journals: DOAJ Articles Journal of Glaciology 66 259 880 886
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Debris-covered glaciers
mountain glaciers
volume scaling methods
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
spellingShingle Debris-covered glaciers
mountain glaciers
volume scaling methods
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
Argha Banerjee
Volume-area scaling for debris-covered glaciers
topic_facet Debris-covered glaciers
mountain glaciers
volume scaling methods
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
description A volume-area scaling relation is commonly used to estimate glacier volume or its future changes on a global scale. The presence of an insulating supraglacial debris cover alters the mass-balance profile of a glacier, potentially modifying the scaling relation. Here, the nature of scaling relations for extensively debris-covered glaciers is investigated. Theoretical arguments suggest that the volume-area scaling exponent for these glaciers is ~7% smaller than that for clean glaciers. This is consistent with the results from flowline-model simulations of idealised glaciers, and the available data from the Himalaya. The best-fit scale factor for debris-covered Himalayan glaciers is ~60% larger compared to that for the clean ones, implying a significantly larger stored ice volume in a debris-covered glacier compared to a clean one having the same area. These results may help improve scaling-based estimates of glacier volume and future glacier changes in regions where debris-covered glaciers are abundant.
format Article in Journal/Newspaper
author Argha Banerjee
author_facet Argha Banerjee
author_sort Argha Banerjee
title Volume-area scaling for debris-covered glaciers
title_short Volume-area scaling for debris-covered glaciers
title_full Volume-area scaling for debris-covered glaciers
title_fullStr Volume-area scaling for debris-covered glaciers
title_full_unstemmed Volume-area scaling for debris-covered glaciers
title_sort volume-area scaling for debris-covered glaciers
publisher Cambridge University Press
publishDate 2020
url https://doi.org/10.1017/jog.2020.69
https://doaj.org/article/817de9ece0c841f398d2f34328aeab24
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology, Vol 66, Pp 880-886 (2020)
op_relation https://www.cambridge.org/core/product/identifier/S0022143020000696/type/journal_article
https://doaj.org/toc/0022-1430
https://doaj.org/toc/1727-5652
doi:10.1017/jog.2020.69
0022-1430
1727-5652
https://doaj.org/article/817de9ece0c841f398d2f34328aeab24
op_doi https://doi.org/10.1017/jog.2020.69
container_title Journal of Glaciology
container_volume 66
container_issue 259
container_start_page 880
op_container_end_page 886
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