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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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 |
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Wageningen UR (University & Research Centre): Digital Library |
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ftunivwagenin |
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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 |
_version_ |
1797587207652900864 |