Arctic Spring Systems Driven by Permafrost Aggradation

Groundwater springs in permafrost regions provide pathways for solutes and dissolved gases to escape from sub-permafrost groundwater systems, which otherwise are completely isolated from the surface environment and atmosphere. Yet, fundamental questions as to the mechanisms driving groundwater flow...

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Published in:Geophysical Research Letters
Main Authors: Hornum, Mikkel Toft, Bense, Victor, van der Ploeg, Martine, Kroon, Aart, Sjöberg, Ylva
Format: Article in Journal/Newspaper
Language:English
Published: 2023
Subjects:
Online Access:https://research.wur.nl/en/publications/arctic-spring-systems-driven-by-permafrost-aggradation
https://doi.org/10.1029/2023GL104719
id ftunivwagenin:oai:library.wur.nl:wurpubs/619462
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spelling ftunivwagenin:oai:library.wur.nl:wurpubs/619462 2024-04-28T08:03:59+00:00 Arctic Spring Systems Driven by Permafrost Aggradation Hornum, Mikkel Toft Bense, Victor van der Ploeg, Martine Kroon, Aart Sjöberg, Ylva 2023 application/pdf https://research.wur.nl/en/publications/arctic-spring-systems-driven-by-permafrost-aggradation https://doi.org/10.1029/2023GL104719 en eng https://edepot.wur.nl/639231 https://research.wur.nl/en/publications/arctic-spring-systems-driven-by-permafrost-aggradation doi:10.1029/2023GL104719 https://creativecommons.org/licenses/by/4.0/ Wageningen University & Research Geophysical Research Letters 50 (2023) 17 ISSN: 0094-8276 Arctic hydrology cryohydrological modeling groundwater springs permafrost pingo springs taliks Article/Letter to editor 2023 ftunivwagenin https://doi.org/10.1029/2023GL104719 2024-04-03T14:26:15Z Groundwater springs in permafrost regions provide pathways for solutes and dissolved gases to escape from sub-permafrost groundwater systems, which otherwise are completely isolated from the surface environment and atmosphere. Yet, fundamental questions as to the mechanisms driving groundwater flow to the surface remain unsolved. In this study, basal permafrost aggradation is explored as a mechanism for generating groundwater flow and driving groundwater spring systems. We employ process-based numerical modeling to test the hypothesis of permafrost-aggradation-driven spring systems in a range of environmental settings. The model results show that permafrost aggradation can generate spring flow on a multi-millennial timescale and with discharge rates up to a couple of liters per second. Permafrost aggradation deserves attention as a groundwater flow driving mechanism in areas of recent glacio-isostatic uplift and glacial retreat. Article in Journal/Newspaper Arctic Arctic permafrost Wageningen UR (University & Research Centre): Digital Library Geophysical Research Letters 50 17
institution Open Polar
collection Wageningen UR (University & Research Centre): Digital Library
op_collection_id ftunivwagenin
language English
topic Arctic hydrology
cryohydrological modeling
groundwater springs
permafrost
pingo springs
taliks
spellingShingle Arctic hydrology
cryohydrological modeling
groundwater springs
permafrost
pingo springs
taliks
Hornum, Mikkel Toft
Bense, Victor
van der Ploeg, Martine
Kroon, Aart
Sjöberg, Ylva
Arctic Spring Systems Driven by Permafrost Aggradation
topic_facet Arctic hydrology
cryohydrological modeling
groundwater springs
permafrost
pingo springs
taliks
description Groundwater springs in permafrost regions provide pathways for solutes and dissolved gases to escape from sub-permafrost groundwater systems, which otherwise are completely isolated from the surface environment and atmosphere. Yet, fundamental questions as to the mechanisms driving groundwater flow to the surface remain unsolved. In this study, basal permafrost aggradation is explored as a mechanism for generating groundwater flow and driving groundwater spring systems. We employ process-based numerical modeling to test the hypothesis of permafrost-aggradation-driven spring systems in a range of environmental settings. The model results show that permafrost aggradation can generate spring flow on a multi-millennial timescale and with discharge rates up to a couple of liters per second. Permafrost aggradation deserves attention as a groundwater flow driving mechanism in areas of recent glacio-isostatic uplift and glacial retreat.
format Article in Journal/Newspaper
author Hornum, Mikkel Toft
Bense, Victor
van der Ploeg, Martine
Kroon, Aart
Sjöberg, Ylva
author_facet Hornum, Mikkel Toft
Bense, Victor
van der Ploeg, Martine
Kroon, Aart
Sjöberg, Ylva
author_sort Hornum, Mikkel Toft
title Arctic Spring Systems Driven by Permafrost Aggradation
title_short Arctic Spring Systems Driven by Permafrost Aggradation
title_full Arctic Spring Systems Driven by Permafrost Aggradation
title_fullStr Arctic Spring Systems Driven by Permafrost Aggradation
title_full_unstemmed Arctic Spring Systems Driven by Permafrost Aggradation
title_sort arctic spring systems driven by permafrost aggradation
publishDate 2023
url https://research.wur.nl/en/publications/arctic-spring-systems-driven-by-permafrost-aggradation
https://doi.org/10.1029/2023GL104719
genre Arctic
Arctic
permafrost
genre_facet Arctic
Arctic
permafrost
op_source Geophysical Research Letters 50 (2023) 17
ISSN: 0094-8276
op_relation https://edepot.wur.nl/639231
https://research.wur.nl/en/publications/arctic-spring-systems-driven-by-permafrost-aggradation
doi:10.1029/2023GL104719
op_rights https://creativecommons.org/licenses/by/4.0/
Wageningen University & Research
op_doi https://doi.org/10.1029/2023GL104719
container_title Geophysical Research Letters
container_volume 50
container_issue 17
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