Scaling-up permafrost thermal measurements in western Alaska using an ecotype approach

Permafrost temperatures are increasing in Alaska due to climate change and in some cases permafrost is thawing and degrading. In areas where degradation has already occurred the effects can be dramatic, resulting in changing ecosystems, carbon release, and damage to infrastructure. However, in many...

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Published in:The Cryosphere
Main Authors: Cable, William L., Romanovsky, Vladimir E., Jorgenson, M. Torre
Language:unknown
Published: 2023
Subjects:
Online Access:http://www.osti.gov/servlets/purl/1375913
https://www.osti.gov/biblio/1375913
https://doi.org/10.5194/tc-10-2517-2016
id ftosti:oai:osti.gov:1375913
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spelling ftosti:oai:osti.gov:1375913 2023-07-30T04:06:13+02:00 Scaling-up permafrost thermal measurements in western Alaska using an ecotype approach Cable, William L. Romanovsky, Vladimir E. Jorgenson, M. Torre 2023-06-26 application/pdf http://www.osti.gov/servlets/purl/1375913 https://www.osti.gov/biblio/1375913 https://doi.org/10.5194/tc-10-2517-2016 unknown http://www.osti.gov/servlets/purl/1375913 https://www.osti.gov/biblio/1375913 https://doi.org/10.5194/tc-10-2517-2016 doi:10.5194/tc-10-2517-2016 58 GEOSCIENCES 2023 ftosti https://doi.org/10.5194/tc-10-2517-2016 2023-07-11T09:20:22Z Permafrost temperatures are increasing in Alaska due to climate change and in some cases permafrost is thawing and degrading. In areas where degradation has already occurred the effects can be dramatic, resulting in changing ecosystems, carbon release, and damage to infrastructure. However, in many areas we lack baseline data, such as subsurface temperatures, needed to assess future changes and potential risk areas. Besides climate, the physical properties of the vegetation cover and subsurface material have a major influence on the thermal state of permafrost. These properties are often directly related to the type of ecosystem overlaying permafrost. In this paper we demonstrate that classifying the landscape into general ecotypes is an effective way to scale up permafrost thermal data collected from field monitoring sites. Additionally, we find that within some ecotypes the absence of a moss layer is indicative of the absence of near-surface permafrost. As a proof of concept, we used the ground temperature data collected from the field sites to recode an ecotype land cover map into a map of mean annual ground temperature ranges at 1 m depth based on analysis and clustering of observed thermal regimes. In conclusion, the map should be useful for decision making with respect to land use and understanding how the landscape might change under future climate scenarios. Other/Unknown Material permafrost Alaska SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy) The Cryosphere 10 5 2517 2532
institution Open Polar
collection SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy)
op_collection_id ftosti
language unknown
topic 58 GEOSCIENCES
spellingShingle 58 GEOSCIENCES
Cable, William L.
Romanovsky, Vladimir E.
Jorgenson, M. Torre
Scaling-up permafrost thermal measurements in western Alaska using an ecotype approach
topic_facet 58 GEOSCIENCES
description Permafrost temperatures are increasing in Alaska due to climate change and in some cases permafrost is thawing and degrading. In areas where degradation has already occurred the effects can be dramatic, resulting in changing ecosystems, carbon release, and damage to infrastructure. However, in many areas we lack baseline data, such as subsurface temperatures, needed to assess future changes and potential risk areas. Besides climate, the physical properties of the vegetation cover and subsurface material have a major influence on the thermal state of permafrost. These properties are often directly related to the type of ecosystem overlaying permafrost. In this paper we demonstrate that classifying the landscape into general ecotypes is an effective way to scale up permafrost thermal data collected from field monitoring sites. Additionally, we find that within some ecotypes the absence of a moss layer is indicative of the absence of near-surface permafrost. As a proof of concept, we used the ground temperature data collected from the field sites to recode an ecotype land cover map into a map of mean annual ground temperature ranges at 1 m depth based on analysis and clustering of observed thermal regimes. In conclusion, the map should be useful for decision making with respect to land use and understanding how the landscape might change under future climate scenarios.
author Cable, William L.
Romanovsky, Vladimir E.
Jorgenson, M. Torre
author_facet Cable, William L.
Romanovsky, Vladimir E.
Jorgenson, M. Torre
author_sort Cable, William L.
title Scaling-up permafrost thermal measurements in western Alaska using an ecotype approach
title_short Scaling-up permafrost thermal measurements in western Alaska using an ecotype approach
title_full Scaling-up permafrost thermal measurements in western Alaska using an ecotype approach
title_fullStr Scaling-up permafrost thermal measurements in western Alaska using an ecotype approach
title_full_unstemmed Scaling-up permafrost thermal measurements in western Alaska using an ecotype approach
title_sort scaling-up permafrost thermal measurements in western alaska using an ecotype approach
publishDate 2023
url http://www.osti.gov/servlets/purl/1375913
https://www.osti.gov/biblio/1375913
https://doi.org/10.5194/tc-10-2517-2016
genre permafrost
Alaska
genre_facet permafrost
Alaska
op_relation http://www.osti.gov/servlets/purl/1375913
https://www.osti.gov/biblio/1375913
https://doi.org/10.5194/tc-10-2517-2016
doi:10.5194/tc-10-2517-2016
op_doi https://doi.org/10.5194/tc-10-2517-2016
container_title The Cryosphere
container_volume 10
container_issue 5
container_start_page 2517
op_container_end_page 2532
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