Climate change impacts on glaciers and runoff in Tien Shan (Central Asia)

Climate-driven changes in glacier-fed streamflow regimes have direct implications on freshwater supply, irrigation and hydropower potential. Reliable information about current and future glaciation and runoff is crucial for water allocation, a complex task in Central Asia, where the collapse of the...

Full description

Bibliographic Details
Published in:Nature Climate Change
Main Authors: Sorg, Annina, Bolch, Tobias, Stoffel, Markus, Solomina, Olga, Beniston, Martin
Format: Article in Journal/Newspaper
Language:English
Published: 2012
Subjects:
Online Access:https://archive-ouverte.unige.ch/unige:22035
id ftunivgeneve:oai:unige.ch:aou:unige:22035
record_format openpolar
spelling ftunivgeneve:oai:unige.ch:aou:unige:22035 2023-10-01T03:58:53+02:00 Climate change impacts on glaciers and runoff in Tien Shan (Central Asia) Sorg, Annina Bolch, Tobias Stoffel, Markus Solomina, Olga Beniston, Martin 2012 https://archive-ouverte.unige.ch/unige:22035 eng eng info:eu-repo/semantics/altIdentifier/doi/10.1038/nclimate1592 info:eu-repo/grantAgreement/EC/FP7/212250/EU/Assessment of Climatic change and impacts on the Quantity and quality of Water/ACQWA https://archive-ouverte.unige.ch/unige:22035 unige:22035 info:eu-repo/semantics/restrictedAccess ISSN: 1758-678X Nature climate change, no. 2 (2012) p. 725-731 info:eu-repo/classification/ddc/333.7-333.9 Climate change Glaciers Water resources info:eu-repo/semantics/article Text Article scientifique info:eu-repo/semantics/publishedVersion 2012 ftunivgeneve https://doi.org/10.1038/nclimate1592 2023-09-07T07:03:42Z Climate-driven changes in glacier-fed streamflow regimes have direct implications on freshwater supply, irrigation and hydropower potential. Reliable information about current and future glaciation and runoff is crucial for water allocation, a complex task in Central Asia, where the collapse of the Soviet Union has transformed previously interdependent republics into autonomous upstream and downstream countries. Although the impacts of climate change on glaciation and runoff have been addressed in previous work undertaken in the Tien Shan (known as the ‘water tower of Central Asia'), a coherent, regional perspective of these findings has not been presented until now. Here we show that glacier shrinkage is most pronounced in peripheral, lower-elevation ranges near the densely populated forelands, where summers are dry and where snow and glacial meltwater is essential for water availability. Shifts of seasonal runoff maxima have already been observed in some rivers, and it is suggested that summer runoff will further decrease in these rivers if precipitation and discharge from thawing permafrost bodies do not compensate sufficiently for water shortfalls. Article in Journal/Newspaper permafrost Université de Genève: Archive ouverte UNIGE Nature Climate Change 2 10 725 731
institution Open Polar
collection Université de Genève: Archive ouverte UNIGE
op_collection_id ftunivgeneve
language English
topic info:eu-repo/classification/ddc/333.7-333.9
Climate change
Glaciers
Water resources
spellingShingle info:eu-repo/classification/ddc/333.7-333.9
Climate change
Glaciers
Water resources
Sorg, Annina
Bolch, Tobias
Stoffel, Markus
Solomina, Olga
Beniston, Martin
Climate change impacts on glaciers and runoff in Tien Shan (Central Asia)
topic_facet info:eu-repo/classification/ddc/333.7-333.9
Climate change
Glaciers
Water resources
description Climate-driven changes in glacier-fed streamflow regimes have direct implications on freshwater supply, irrigation and hydropower potential. Reliable information about current and future glaciation and runoff is crucial for water allocation, a complex task in Central Asia, where the collapse of the Soviet Union has transformed previously interdependent republics into autonomous upstream and downstream countries. Although the impacts of climate change on glaciation and runoff have been addressed in previous work undertaken in the Tien Shan (known as the ‘water tower of Central Asia'), a coherent, regional perspective of these findings has not been presented until now. Here we show that glacier shrinkage is most pronounced in peripheral, lower-elevation ranges near the densely populated forelands, where summers are dry and where snow and glacial meltwater is essential for water availability. Shifts of seasonal runoff maxima have already been observed in some rivers, and it is suggested that summer runoff will further decrease in these rivers if precipitation and discharge from thawing permafrost bodies do not compensate sufficiently for water shortfalls.
format Article in Journal/Newspaper
author Sorg, Annina
Bolch, Tobias
Stoffel, Markus
Solomina, Olga
Beniston, Martin
author_facet Sorg, Annina
Bolch, Tobias
Stoffel, Markus
Solomina, Olga
Beniston, Martin
author_sort Sorg, Annina
title Climate change impacts on glaciers and runoff in Tien Shan (Central Asia)
title_short Climate change impacts on glaciers and runoff in Tien Shan (Central Asia)
title_full Climate change impacts on glaciers and runoff in Tien Shan (Central Asia)
title_fullStr Climate change impacts on glaciers and runoff in Tien Shan (Central Asia)
title_full_unstemmed Climate change impacts on glaciers and runoff in Tien Shan (Central Asia)
title_sort climate change impacts on glaciers and runoff in tien shan (central asia)
publishDate 2012
url https://archive-ouverte.unige.ch/unige:22035
genre permafrost
genre_facet permafrost
op_source ISSN: 1758-678X
Nature climate change, no. 2 (2012) p. 725-731
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1038/nclimate1592
info:eu-repo/grantAgreement/EC/FP7/212250/EU/Assessment of Climatic change and impacts on the Quantity and quality of Water/ACQWA
https://archive-ouverte.unige.ch/unige:22035
unige:22035
op_rights info:eu-repo/semantics/restrictedAccess
op_doi https://doi.org/10.1038/nclimate1592
container_title Nature Climate Change
container_volume 2
container_issue 10
container_start_page 725
op_container_end_page 731
_version_ 1778532118444376064