Chapter 8 The Status and Role of the alpine Cryosphere in Central Asia

The alpine cryosphere including snow, glaciers and permafrost are critical to water management in the Aral Sea Basin (ASB) and larger Central Asia (CA) under changing climate: as they store large amounts of water in its solid forms. Most cryospheric components in the Aral Sea Basin are close to melt...

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Main Authors: Bolch, Tobias, Hoelzle, Martin, Barandun, Martina
Format: Book
Language:English
Published: Taylor & Francis 2019
Subjects:
geo
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spelling fttriple:oai:gotriple.eu:10670/1.n1buu6 2023-05-15T17:57:17+02:00 Chapter 8 The Status and Role of the alpine Cryosphere in Central Asia Bolch, Tobias Hoelzle, Martin Barandun, Martina 2019-01-01 https://openresearchlibrary.org/ext/api/media/ed9db67b-ff10-4cc5-ab9d-a536b62cc768/assets/external_content.pdf https://openresearchlibrary.org/viewer/ed9db67b-ff10-4cc5-ab9d-a536b62cc768 en eng Taylor & Francis ISBN:9781138348882 10670/1.n1buu6 https://openresearchlibrary.org/ext/api/media/ed9db67b-ff10-4cc5-ab9d-a536b62cc768/assets/external_content.pdf https://openresearchlibrary.org/viewer/ed9db67b-ff10-4cc5-ab9d-a536b62cc768 lic_creative-commons Open Research Library geo envir Book https://vocabularies.coar-repositories.org/resource_types/c_2f33/ 2019 fttriple 2023-01-22T17:15:34Z The alpine cryosphere including snow, glaciers and permafrost are critical to water management in the Aral Sea Basin (ASB) and larger Central Asia (CA) under changing climate: as they store large amounts of water in its solid forms. Most cryospheric components in the Aral Sea Basin are close to melting point, and hence very vulnerable to a slight increase in air temperature with significant consequences to long-term water availability and to water resources variability and extremes. Current knowledge about different components of cryosphere and their connection to climate in the Basin and in the entire Central Asia, varies. While it is advanced in the topics of snow and glaciers, knowledge on permafrost it rather limited. Observed trends in runoff point in the direction of increasing water availability in July and August at least until mid-century and increasing possibility for water storage in reservoirs and aquifers. However, eventually this will change as glaciers waste away. Future runoff may change considerably after mid-century and start to decline if not compensated by increasing precipitation. Cryosphere monitoring systems are the basis for sound estimates of water availability and water-related hazards associated with snow, glaciers and permafrost. They require a well-distributed observational network for all cryospheric variables. Such systems need to be re-established in the Basin after the breakup of the Soviet Union in the early 1990s. This process is slowly emerging in the region. Collaboration between local operational hydro-meteorological services and academic sector, and with international research networks may improving the observing capabilities in high mountain regions of CA Asia in general and the ASB specifically. Book permafrost Unknown
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic geo
envir
spellingShingle geo
envir
Bolch, Tobias
Hoelzle, Martin
Barandun, Martina
Chapter 8 The Status and Role of the alpine Cryosphere in Central Asia
topic_facet geo
envir
description The alpine cryosphere including snow, glaciers and permafrost are critical to water management in the Aral Sea Basin (ASB) and larger Central Asia (CA) under changing climate: as they store large amounts of water in its solid forms. Most cryospheric components in the Aral Sea Basin are close to melting point, and hence very vulnerable to a slight increase in air temperature with significant consequences to long-term water availability and to water resources variability and extremes. Current knowledge about different components of cryosphere and their connection to climate in the Basin and in the entire Central Asia, varies. While it is advanced in the topics of snow and glaciers, knowledge on permafrost it rather limited. Observed trends in runoff point in the direction of increasing water availability in July and August at least until mid-century and increasing possibility for water storage in reservoirs and aquifers. However, eventually this will change as glaciers waste away. Future runoff may change considerably after mid-century and start to decline if not compensated by increasing precipitation. Cryosphere monitoring systems are the basis for sound estimates of water availability and water-related hazards associated with snow, glaciers and permafrost. They require a well-distributed observational network for all cryospheric variables. Such systems need to be re-established in the Basin after the breakup of the Soviet Union in the early 1990s. This process is slowly emerging in the region. Collaboration between local operational hydro-meteorological services and academic sector, and with international research networks may improving the observing capabilities in high mountain regions of CA Asia in general and the ASB specifically.
format Book
author Bolch, Tobias
Hoelzle, Martin
Barandun, Martina
author_facet Bolch, Tobias
Hoelzle, Martin
Barandun, Martina
author_sort Bolch, Tobias
title Chapter 8 The Status and Role of the alpine Cryosphere in Central Asia
title_short Chapter 8 The Status and Role of the alpine Cryosphere in Central Asia
title_full Chapter 8 The Status and Role of the alpine Cryosphere in Central Asia
title_fullStr Chapter 8 The Status and Role of the alpine Cryosphere in Central Asia
title_full_unstemmed Chapter 8 The Status and Role of the alpine Cryosphere in Central Asia
title_sort chapter 8 the status and role of the alpine cryosphere in central asia
publisher Taylor & Francis
publishDate 2019
url https://openresearchlibrary.org/ext/api/media/ed9db67b-ff10-4cc5-ab9d-a536b62cc768/assets/external_content.pdf
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genre permafrost
genre_facet permafrost
op_source Open Research Library
op_relation ISBN:9781138348882
10670/1.n1buu6
https://openresearchlibrary.org/ext/api/media/ed9db67b-ff10-4cc5-ab9d-a536b62cc768/assets/external_content.pdf
https://openresearchlibrary.org/viewer/ed9db67b-ff10-4cc5-ab9d-a536b62cc768
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