Continentality determines warming or cooling impact of heavy rainfall events on permafrost

Permafrost thaw can cause an intensification of climate change through the release of carbon as greenhouse gases. While the effect of air temperature on permafrost thaw is well quantified, the effect of rainfall is highly variable and not well understood. Here, we provide a literature review of stud...

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Published in:Nature Communications
Main Authors: Hamm, Alexandra, Magnússon, Rúna, Khattak, Ahmad Jan, Frampton, Andrew
Format: Article in Journal/Newspaper
Language:English
Published: 2023
Subjects:
Online Access:https://research.wur.nl/en/publications/continentality-determines-warming-or-cooling-impact-of-heavy-rain
https://doi.org/10.1038/s41467-023-39325-4
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spelling ftunivwagenin:oai:library.wur.nl:wurpubs/616089 2024-04-28T07:53:14+00:00 Continentality determines warming or cooling impact of heavy rainfall events on permafrost Hamm, Alexandra Magnússon, Rúna Khattak, Ahmad Jan Frampton, Andrew 2023 application/pdf https://research.wur.nl/en/publications/continentality-determines-warming-or-cooling-impact-of-heavy-rain https://doi.org/10.1038/s41467-023-39325-4 en eng https://edepot.wur.nl/633128 https://research.wur.nl/en/publications/continentality-determines-warming-or-cooling-impact-of-heavy-rain doi:10.1038/s41467-023-39325-4 https://creativecommons.org/licenses/by/4.0/ Wageningen University & Research Nature Communications 14 (2023) 1 ISSN: 2041-1723 Life Science Article/Letter to editor 2023 ftunivwagenin https://doi.org/10.1038/s41467-023-39325-4 2024-04-03T14:34:17Z Permafrost thaw can cause an intensification of climate change through the release of carbon as greenhouse gases. While the effect of air temperature on permafrost thaw is well quantified, the effect of rainfall is highly variable and not well understood. Here, we provide a literature review of studies reporting on effects of rainfall on ground temperatures in permafrost environments and use a numerical model to explore the underlying physical mechanisms under different climatic conditions. Both the evaluated body of literature and the model simulations indicate that continental climates are likely to show a warming of the subsoil and hence increased end of season active layer thickness, while maritime climates tend to respond with a slight cooling effect. This suggests that dry regions with warm summers are prone to more rapid permafrost degradation under increased occurrences of heavy rainfall events in the future, which can potentially accelerate the permafrost carbon feedback. Article in Journal/Newspaper Active layer thickness permafrost Wageningen UR (University & Research Centre): Digital Library Nature Communications 14 1
institution Open Polar
collection Wageningen UR (University & Research Centre): Digital Library
op_collection_id ftunivwagenin
language English
topic Life Science
spellingShingle Life Science
Hamm, Alexandra
Magnússon, Rúna
Khattak, Ahmad Jan
Frampton, Andrew
Continentality determines warming or cooling impact of heavy rainfall events on permafrost
topic_facet Life Science
description Permafrost thaw can cause an intensification of climate change through the release of carbon as greenhouse gases. While the effect of air temperature on permafrost thaw is well quantified, the effect of rainfall is highly variable and not well understood. Here, we provide a literature review of studies reporting on effects of rainfall on ground temperatures in permafrost environments and use a numerical model to explore the underlying physical mechanisms under different climatic conditions. Both the evaluated body of literature and the model simulations indicate that continental climates are likely to show a warming of the subsoil and hence increased end of season active layer thickness, while maritime climates tend to respond with a slight cooling effect. This suggests that dry regions with warm summers are prone to more rapid permafrost degradation under increased occurrences of heavy rainfall events in the future, which can potentially accelerate the permafrost carbon feedback.
format Article in Journal/Newspaper
author Hamm, Alexandra
Magnússon, Rúna
Khattak, Ahmad Jan
Frampton, Andrew
author_facet Hamm, Alexandra
Magnússon, Rúna
Khattak, Ahmad Jan
Frampton, Andrew
author_sort Hamm, Alexandra
title Continentality determines warming or cooling impact of heavy rainfall events on permafrost
title_short Continentality determines warming or cooling impact of heavy rainfall events on permafrost
title_full Continentality determines warming or cooling impact of heavy rainfall events on permafrost
title_fullStr Continentality determines warming or cooling impact of heavy rainfall events on permafrost
title_full_unstemmed Continentality determines warming or cooling impact of heavy rainfall events on permafrost
title_sort continentality determines warming or cooling impact of heavy rainfall events on permafrost
publishDate 2023
url https://research.wur.nl/en/publications/continentality-determines-warming-or-cooling-impact-of-heavy-rain
https://doi.org/10.1038/s41467-023-39325-4
genre Active layer thickness
permafrost
genre_facet Active layer thickness
permafrost
op_source Nature Communications 14 (2023) 1
ISSN: 2041-1723
op_relation https://edepot.wur.nl/633128
https://research.wur.nl/en/publications/continentality-determines-warming-or-cooling-impact-of-heavy-rain
doi:10.1038/s41467-023-39325-4
op_rights https://creativecommons.org/licenses/by/4.0/
Wageningen University & Research
op_doi https://doi.org/10.1038/s41467-023-39325-4
container_title Nature Communications
container_volume 14
container_issue 1
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