Tundra vegetation change and impacts on permafrost

Tundra vegetation productivity and composition are responding rapidly to climatic changes in the Arctic. These changes can, in turn, mitigate or amplify permafrost thaw. In this Review, we synthesize remotely sensed and field-observed vegetation change across the tundra biome, and outline how these...

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Published in:Nature Reviews Earth & Environment
Other Authors: Heijmans, Monique M. P. D. (author), Magnússon, Rúna Í. (author), Lara, Mark J. (author), Frost, Gerald V. (author), Myers-Smith, Isla H. (author), van Huissteden, Jacobus (author), Jorgenson, M. Torre (author), Fedorov, Alexander N. (author), Epstein, Howard E. (author), Lawrence, David M. (author), Limpens, Juul (author)
Format: Article in Journal/Newspaper
Language:English
Published: 2022
Subjects:
Ice
Online Access:https://doi.org/10.1038/s43017-021-00233-0
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spelling ftncar:oai:drupal-site.org:articles_25035 2024-04-28T08:07:14+00:00 Tundra vegetation change and impacts on permafrost Heijmans, Monique M. P. D. (author) Magnússon, Rúna Í. (author) Lara, Mark J. (author) Frost, Gerald V. (author) Myers-Smith, Isla H. (author) van Huissteden, Jacobus (author) Jorgenson, M. Torre (author) Fedorov, Alexander N. (author) Epstein, Howard E. (author) Lawrence, David M. (author) Limpens, Juul (author) 2022-01-11 https://doi.org/10.1038/s43017-021-00233-0 en eng Nature Reviews Earth & Environment--Nat Rev Earth Environ--2662-138X articles:25035 doi:10.1038/s43017-021-00233-0 ark:/85065/d7n01b2f Copyright 2022 Springer Nature Ltd. article Text 2022 ftncar https://doi.org/10.1038/s43017-021-00233-0 2024-04-04T17:34:52Z Tundra vegetation productivity and composition are responding rapidly to climatic changes in the Arctic. These changes can, in turn, mitigate or amplify permafrost thaw. In this Review, we synthesize remotely sensed and field-observed vegetation change across the tundra biome, and outline how these shifts could influence permafrost thaw. Permafrost ice content appears to be an important control on local vegetation changes; woody vegetation generally increases in ice-poor uplands, whereas replacement of woody vegetation by (aquatic) graminoids following abrupt permafrost thaw is more frequent in ice-rich Arctic lowlands. These locally observed vegetation changes contribute to regional satellite-observed greening trends, although the interpretation of greening and browning is complicated. Increases in vegetation cover and height generally mitigate permafrost thaw in summer, yet, increase annual soil temperatures through snow-related winter soil warming effects. Strong vegetation-soil feedbacks currently alleviate the consequences of thaw-related disturbances. However, if the increasing scale and frequency of disturbances in a warming Arctic exceeds the capacity for vegetation and permafrost recovery, changes to Arctic ecosystems could be irreversible. To better disentangle vegetation-soil-permafrost interactions, ecological field studies remain crucial, but require better integration with geophysical assessments. Article in Journal/Newspaper Arctic Ice permafrost Tundra OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research) Nature Reviews Earth & Environment 3 1 68 84
institution Open Polar
collection OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research)
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language English
description Tundra vegetation productivity and composition are responding rapidly to climatic changes in the Arctic. These changes can, in turn, mitigate or amplify permafrost thaw. In this Review, we synthesize remotely sensed and field-observed vegetation change across the tundra biome, and outline how these shifts could influence permafrost thaw. Permafrost ice content appears to be an important control on local vegetation changes; woody vegetation generally increases in ice-poor uplands, whereas replacement of woody vegetation by (aquatic) graminoids following abrupt permafrost thaw is more frequent in ice-rich Arctic lowlands. These locally observed vegetation changes contribute to regional satellite-observed greening trends, although the interpretation of greening and browning is complicated. Increases in vegetation cover and height generally mitigate permafrost thaw in summer, yet, increase annual soil temperatures through snow-related winter soil warming effects. Strong vegetation-soil feedbacks currently alleviate the consequences of thaw-related disturbances. However, if the increasing scale and frequency of disturbances in a warming Arctic exceeds the capacity for vegetation and permafrost recovery, changes to Arctic ecosystems could be irreversible. To better disentangle vegetation-soil-permafrost interactions, ecological field studies remain crucial, but require better integration with geophysical assessments.
author2 Heijmans, Monique M. P. D. (author)
Magnússon, Rúna Í. (author)
Lara, Mark J. (author)
Frost, Gerald V. (author)
Myers-Smith, Isla H. (author)
van Huissteden, Jacobus (author)
Jorgenson, M. Torre (author)
Fedorov, Alexander N. (author)
Epstein, Howard E. (author)
Lawrence, David M. (author)
Limpens, Juul (author)
format Article in Journal/Newspaper
title Tundra vegetation change and impacts on permafrost
spellingShingle Tundra vegetation change and impacts on permafrost
title_short Tundra vegetation change and impacts on permafrost
title_full Tundra vegetation change and impacts on permafrost
title_fullStr Tundra vegetation change and impacts on permafrost
title_full_unstemmed Tundra vegetation change and impacts on permafrost
title_sort tundra vegetation change and impacts on permafrost
publishDate 2022
url https://doi.org/10.1038/s43017-021-00233-0
genre Arctic
Ice
permafrost
Tundra
genre_facet Arctic
Ice
permafrost
Tundra
op_relation Nature Reviews Earth & Environment--Nat Rev Earth Environ--2662-138X
articles:25035
doi:10.1038/s43017-021-00233-0
ark:/85065/d7n01b2f
op_rights Copyright 2022 Springer Nature Ltd.
op_doi https://doi.org/10.1038/s43017-021-00233-0
container_title Nature Reviews Earth & Environment
container_volume 3
container_issue 1
container_start_page 68
op_container_end_page 84
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