Permafrost evolution in a mountain catchment near Santiago de Chile

The Chilean Central Andes near Santiago are a semi-arid region with substantial frozen water reserves in their high altitude cryosphere. Millions of people depend on the Andean cryosphere for freshwater supply. Over the last sixty years, global warming has altered the mountains' water balance,...

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Published in:Journal of South American Earth Sciences
Main Authors: Ruiz Pereira, S., Marquardt, C., Beriain, E., Lambert, F.
Format: Article in Journal/Newspaper
Language:English
Published: 2023
Subjects:
Online Access:https://repositorio.uc.cl/handle/11534/70362
https://doi.org/10.1016/J.JSAMES.2021.103293
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spelling ftpunivcchile:oai:repositorio.uc.cl:11534/70362 2024-09-15T18:29:24+00:00 Permafrost evolution in a mountain catchment near Santiago de Chile Ruiz Pereira, S. Marquardt, C. Beriain, E. Lambert, F. 2023-05-19T20:50:51Z https://repositorio.uc.cl/handle/11534/70362 https://doi.org/10.1016/J.JSAMES.2021.103293 en eng doi:10.1016/J.JSAMES.2021.103293 https://repositorio.uc.cl/handle/11534/70362 artículo 2023 ftpunivcchile https://doi.org/10.1016/J.JSAMES.2021.103293 2024-07-08T23:47:41Z The Chilean Central Andes near Santiago are a semi-arid region with substantial frozen water reserves in their high altitude cryosphere. Millions of people depend on the Andean cryosphere for freshwater supply. Over the last sixty years, global warming has altered the mountains' water balance, as the temperature rose, precipitation decreased, and deglacierization exposed hundreds of square kilometers. The distribution of solid water stored in soil permafrost and the potential effects of climate change on it are unknown. Here, we map favorable spots for permafrost occurrence at the "Monos de Agua" catchment, Aconcagua basin at 33 degrees S, between 3600 and 5100 m a.s.l. We identify these "cold spots" based on ground surface temperature and incoming solar radiation between 2017 and 2019. We suggest that these locations currently present permafrost and frozen water might actually be there. We confirmed a body of frozen water at one of these cold spots using an electrical resistivity survey. Our mapping suggests that at least 15 +/- 7% of the catchment's surface is underlain by permafrost. Permafrost occurrence begins around 3600 m a.s.l. with low probability and only at locations with favorable conditions of low exposure and isolation. Permafrost occurrence probability increases with altitude, with the largest fraction present above 4200 m a.s.l. Our results suggest that the permafrost area in this region will decrease between 13 and 87% by the end of the century under the future global warming RCP scenarios. This event represents new challenges for the hydrological memory and water security planning in the Chilean Central Andes. Article in Journal/Newspaper permafrost Pontificia Universidad Católica de Chile: Repositorio UC Journal of South American Earth Sciences 109 103293
institution Open Polar
collection Pontificia Universidad Católica de Chile: Repositorio UC
op_collection_id ftpunivcchile
language English
description The Chilean Central Andes near Santiago are a semi-arid region with substantial frozen water reserves in their high altitude cryosphere. Millions of people depend on the Andean cryosphere for freshwater supply. Over the last sixty years, global warming has altered the mountains' water balance, as the temperature rose, precipitation decreased, and deglacierization exposed hundreds of square kilometers. The distribution of solid water stored in soil permafrost and the potential effects of climate change on it are unknown. Here, we map favorable spots for permafrost occurrence at the "Monos de Agua" catchment, Aconcagua basin at 33 degrees S, between 3600 and 5100 m a.s.l. We identify these "cold spots" based on ground surface temperature and incoming solar radiation between 2017 and 2019. We suggest that these locations currently present permafrost and frozen water might actually be there. We confirmed a body of frozen water at one of these cold spots using an electrical resistivity survey. Our mapping suggests that at least 15 +/- 7% of the catchment's surface is underlain by permafrost. Permafrost occurrence begins around 3600 m a.s.l. with low probability and only at locations with favorable conditions of low exposure and isolation. Permafrost occurrence probability increases with altitude, with the largest fraction present above 4200 m a.s.l. Our results suggest that the permafrost area in this region will decrease between 13 and 87% by the end of the century under the future global warming RCP scenarios. This event represents new challenges for the hydrological memory and water security planning in the Chilean Central Andes.
format Article in Journal/Newspaper
author Ruiz Pereira, S.
Marquardt, C.
Beriain, E.
Lambert, F.
spellingShingle Ruiz Pereira, S.
Marquardt, C.
Beriain, E.
Lambert, F.
Permafrost evolution in a mountain catchment near Santiago de Chile
author_facet Ruiz Pereira, S.
Marquardt, C.
Beriain, E.
Lambert, F.
author_sort Ruiz Pereira, S.
title Permafrost evolution in a mountain catchment near Santiago de Chile
title_short Permafrost evolution in a mountain catchment near Santiago de Chile
title_full Permafrost evolution in a mountain catchment near Santiago de Chile
title_fullStr Permafrost evolution in a mountain catchment near Santiago de Chile
title_full_unstemmed Permafrost evolution in a mountain catchment near Santiago de Chile
title_sort permafrost evolution in a mountain catchment near santiago de chile
publishDate 2023
url https://repositorio.uc.cl/handle/11534/70362
https://doi.org/10.1016/J.JSAMES.2021.103293
genre permafrost
genre_facet permafrost
op_relation doi:10.1016/J.JSAMES.2021.103293
https://repositorio.uc.cl/handle/11534/70362
op_doi https://doi.org/10.1016/J.JSAMES.2021.103293
container_title Journal of South American Earth Sciences
container_volume 109
container_start_page 103293
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