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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Cambridge University Press
2020
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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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1766049128526118912 |