Snowfall in the Himalayas: an uncertain future from a little-known past

Snow and ice provide large amounts of meltwater to the Indus, Ganges and Brahmaputra rivers. This study combines present-day observations and reanalysis data with climate model projections to estimate the amount of snow falling over the basins today and in the last decades of the 21st century. Estim...

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Published in:The Cryosphere
Main Authors: E. Viste, A. Sorteberg
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2015
Subjects:
geo
Online Access:https://doi.org/10.5194/tc-9-1147-2015
http://www.the-cryosphere.net/9/1147/2015/tc-9-1147-2015.pdf
https://doaj.org/article/6250840ba0f64423b729bc5ec3e4f8d6
id fttriple:oai:gotriple.eu:oai:doaj.org/article:6250840ba0f64423b729bc5ec3e4f8d6
record_format openpolar
spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:6250840ba0f64423b729bc5ec3e4f8d6 2023-05-15T18:32:22+02:00 Snowfall in the Himalayas: an uncertain future from a little-known past E. Viste A. Sorteberg 2015-06-01 https://doi.org/10.5194/tc-9-1147-2015 http://www.the-cryosphere.net/9/1147/2015/tc-9-1147-2015.pdf https://doaj.org/article/6250840ba0f64423b729bc5ec3e4f8d6 en eng Copernicus Publications 1994-0416 1994-0424 doi:10.5194/tc-9-1147-2015 http://www.the-cryosphere.net/9/1147/2015/tc-9-1147-2015.pdf https://doaj.org/article/6250840ba0f64423b729bc5ec3e4f8d6 undefined The Cryosphere, Vol 9, Iss 3, Pp 1147-1167 (2015) geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2015 fttriple https://doi.org/10.5194/tc-9-1147-2015 2023-01-22T19:11:20Z Snow and ice provide large amounts of meltwater to the Indus, Ganges and Brahmaputra rivers. This study combines present-day observations and reanalysis data with climate model projections to estimate the amount of snow falling over the basins today and in the last decades of the 21st century. Estimates of present-day snowfall based on a combination of temperature and precipitation from reanalysis data and observations vary by factors of 2–4. The spread is large, not just between the reanalysis and the observations but also between the different observational data sets. With the strongest anthropogenic forcing scenario (RCP8.5), the climate models project reductions in annual snowfall by 30–50% in the Indus Basin, 50–60% in the Ganges Basin and 50–70% in the Brahmaputra Basin by 2071–2100. The reduction is due to increasing temperatures, as the mean of the models show constant or increasing precipitation throughout the year in most of the region. With the strongest anthropogenic forcing scenario, the mean elevation where rain changes to snow – the rain/snow line – creeps upward by 400–900 m, in most of the region by 700–900 meters. The largest relative change in snowfall is seen in the upper westernmost sub-basins of the Brahmaputra. With the strongest forcing scenario, most of this region will have temperatures above freezing, especially in the summer. The projected reduction in annual snowfall is 65–75%. In the upper Indus, the effect of a warmer climate on snowfall is less extreme, as most of the terrain is high enough to have temperatures sufficiently far below freezing today. A 20–40% reduction in annual snowfall is projected. Article in Journal/Newspaper The Cryosphere Unknown The Cryosphere 9 3 1147 1167
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic geo
envir
spellingShingle geo
envir
E. Viste
A. Sorteberg
Snowfall in the Himalayas: an uncertain future from a little-known past
topic_facet geo
envir
description Snow and ice provide large amounts of meltwater to the Indus, Ganges and Brahmaputra rivers. This study combines present-day observations and reanalysis data with climate model projections to estimate the amount of snow falling over the basins today and in the last decades of the 21st century. Estimates of present-day snowfall based on a combination of temperature and precipitation from reanalysis data and observations vary by factors of 2–4. The spread is large, not just between the reanalysis and the observations but also between the different observational data sets. With the strongest anthropogenic forcing scenario (RCP8.5), the climate models project reductions in annual snowfall by 30–50% in the Indus Basin, 50–60% in the Ganges Basin and 50–70% in the Brahmaputra Basin by 2071–2100. The reduction is due to increasing temperatures, as the mean of the models show constant or increasing precipitation throughout the year in most of the region. With the strongest anthropogenic forcing scenario, the mean elevation where rain changes to snow – the rain/snow line – creeps upward by 400–900 m, in most of the region by 700–900 meters. The largest relative change in snowfall is seen in the upper westernmost sub-basins of the Brahmaputra. With the strongest forcing scenario, most of this region will have temperatures above freezing, especially in the summer. The projected reduction in annual snowfall is 65–75%. In the upper Indus, the effect of a warmer climate on snowfall is less extreme, as most of the terrain is high enough to have temperatures sufficiently far below freezing today. A 20–40% reduction in annual snowfall is projected.
format Article in Journal/Newspaper
author E. Viste
A. Sorteberg
author_facet E. Viste
A. Sorteberg
author_sort E. Viste
title Snowfall in the Himalayas: an uncertain future from a little-known past
title_short Snowfall in the Himalayas: an uncertain future from a little-known past
title_full Snowfall in the Himalayas: an uncertain future from a little-known past
title_fullStr Snowfall in the Himalayas: an uncertain future from a little-known past
title_full_unstemmed Snowfall in the Himalayas: an uncertain future from a little-known past
title_sort snowfall in the himalayas: an uncertain future from a little-known past
publisher Copernicus Publications
publishDate 2015
url https://doi.org/10.5194/tc-9-1147-2015
http://www.the-cryosphere.net/9/1147/2015/tc-9-1147-2015.pdf
https://doaj.org/article/6250840ba0f64423b729bc5ec3e4f8d6
genre The Cryosphere
genre_facet The Cryosphere
op_source The Cryosphere, Vol 9, Iss 3, Pp 1147-1167 (2015)
op_relation 1994-0416
1994-0424
doi:10.5194/tc-9-1147-2015
http://www.the-cryosphere.net/9/1147/2015/tc-9-1147-2015.pdf
https://doaj.org/article/6250840ba0f64423b729bc5ec3e4f8d6
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op_doi https://doi.org/10.5194/tc-9-1147-2015
container_title The Cryosphere
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container_issue 3
container_start_page 1147
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