Future climate warming and changes to mountain permafrost in the Bolivian Andes

Water resources in many of the world’s arid mountain ranges are threatened by climate change, and in parts of the South American Andes this is exacerbated by glacier recession and population growth. Alternative sources of water, such as more resilient permafrost features (e.g. rock glaciers), are ex...

Full description

Bibliographic Details
Published in:Climatic Change
Main Authors: Rangecroft, Sally, Suggitt, Andrew J., Anderson, Karen, Harrison, Stephan
Format: Text
Language:English
Published: Springer Netherlands 2016
Subjects:
Online Access:http://www.ncbi.nlm.nih.gov/pmc/articles/PMC7175727/
https://doi.org/10.1007/s10584-016-1655-8
id ftpubmed:oai:pubmedcentral.nih.gov:7175727
record_format openpolar
spelling ftpubmed:oai:pubmedcentral.nih.gov:7175727 2023-05-15T17:55:37+02:00 Future climate warming and changes to mountain permafrost in the Bolivian Andes Rangecroft, Sally Suggitt, Andrew J. Anderson, Karen Harrison, Stephan 2016-04-13 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC7175727/ https://doi.org/10.1007/s10584-016-1655-8 en eng Springer Netherlands http://www.ncbi.nlm.nih.gov/pmc/articles/PMC7175727/ http://dx.doi.org/10.1007/s10584-016-1655-8 © The Author(s) 2016 Open Access This article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. CC-BY Article Text 2016 ftpubmed https://doi.org/10.1007/s10584-016-1655-8 2020-05-03T00:33:37Z Water resources in many of the world’s arid mountain ranges are threatened by climate change, and in parts of the South American Andes this is exacerbated by glacier recession and population growth. Alternative sources of water, such as more resilient permafrost features (e.g. rock glaciers), are expected to become increasingly important as current warming continues. Assessments of current and future permafrost extent under climate change are not available for the Southern Hemisphere, yet are required to inform decision making over future water supply and climate change adaptation strategies. Here, downscaled model outputs were used to calculate the projected changes in permafrost extent for a first-order assessment of an example region, the Bolivian Andes. Using the 0 °C mean annual air temperature as a proxy for permafrost extent, these projections show that permafrost areas will shrink from present day extent by up to 95 % under warming projected for the 2050s and by 99 % for the 2080s (under the IPCC A1B scenario, given equilibrium conditions). Using active rock glaciers as a proxy for the lower limit of permafrost extent, we also estimate that projected temperature changes would drive a near total loss of currently active rock glaciers in this region by the end of the century. In conjunction with glacier recession, a loss of permafrost extent of this magnitude represents a water security problem for the latter part of the 21st century, and it is likely that this will have negative effects on one of South America’s fastest growing cities (La Paz), with similar implications for other arid mountain regions. Text permafrost PubMed Central (PMC) Climatic Change 137 1-2 231 243
institution Open Polar
collection PubMed Central (PMC)
op_collection_id ftpubmed
language English
topic Article
spellingShingle Article
Rangecroft, Sally
Suggitt, Andrew J.
Anderson, Karen
Harrison, Stephan
Future climate warming and changes to mountain permafrost in the Bolivian Andes
topic_facet Article
description Water resources in many of the world’s arid mountain ranges are threatened by climate change, and in parts of the South American Andes this is exacerbated by glacier recession and population growth. Alternative sources of water, such as more resilient permafrost features (e.g. rock glaciers), are expected to become increasingly important as current warming continues. Assessments of current and future permafrost extent under climate change are not available for the Southern Hemisphere, yet are required to inform decision making over future water supply and climate change adaptation strategies. Here, downscaled model outputs were used to calculate the projected changes in permafrost extent for a first-order assessment of an example region, the Bolivian Andes. Using the 0 °C mean annual air temperature as a proxy for permafrost extent, these projections show that permafrost areas will shrink from present day extent by up to 95 % under warming projected for the 2050s and by 99 % for the 2080s (under the IPCC A1B scenario, given equilibrium conditions). Using active rock glaciers as a proxy for the lower limit of permafrost extent, we also estimate that projected temperature changes would drive a near total loss of currently active rock glaciers in this region by the end of the century. In conjunction with glacier recession, a loss of permafrost extent of this magnitude represents a water security problem for the latter part of the 21st century, and it is likely that this will have negative effects on one of South America’s fastest growing cities (La Paz), with similar implications for other arid mountain regions.
format Text
author Rangecroft, Sally
Suggitt, Andrew J.
Anderson, Karen
Harrison, Stephan
author_facet Rangecroft, Sally
Suggitt, Andrew J.
Anderson, Karen
Harrison, Stephan
author_sort Rangecroft, Sally
title Future climate warming and changes to mountain permafrost in the Bolivian Andes
title_short Future climate warming and changes to mountain permafrost in the Bolivian Andes
title_full Future climate warming and changes to mountain permafrost in the Bolivian Andes
title_fullStr Future climate warming and changes to mountain permafrost in the Bolivian Andes
title_full_unstemmed Future climate warming and changes to mountain permafrost in the Bolivian Andes
title_sort future climate warming and changes to mountain permafrost in the bolivian andes
publisher Springer Netherlands
publishDate 2016
url http://www.ncbi.nlm.nih.gov/pmc/articles/PMC7175727/
https://doi.org/10.1007/s10584-016-1655-8
genre permafrost
genre_facet permafrost
op_relation http://www.ncbi.nlm.nih.gov/pmc/articles/PMC7175727/
http://dx.doi.org/10.1007/s10584-016-1655-8
op_rights © The Author(s) 2016
Open Access This article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made.
op_rightsnorm CC-BY
op_doi https://doi.org/10.1007/s10584-016-1655-8
container_title Climatic Change
container_volume 137
container_issue 1-2
container_start_page 231
op_container_end_page 243
_version_ 1766163582220763136