Rapid warming and degradation of mountain permafrost in Norway and Iceland

With the EU-funded PACE (Permafrost and Climate in Europe) project at the turn of this century, several deep boreholes (100 m + ) were drilled in European mountain sites, including in mainland Norway, Svalbard and Sweden. During other projects from 2004 and the International Polar Year (IPY) period...

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Published in:The Cryosphere
Main Authors: Etzelmüller, Bernd, Isaksen, Ketil, Czekirda, Justyna, Westermann, Sebastian, Hilbich, Christin, Hauck, Christian
Format: Text
Language:English
Published: 2023
Subjects:
IPY
Online Access:https://doi.org/10.5194/tc-17-5477-2023
https://tc.copernicus.org/articles/17/5477/2023/
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spelling ftcopernicus:oai:publications.copernicus.org:tc110241 2024-01-21T10:07:11+01:00 Rapid warming and degradation of mountain permafrost in Norway and Iceland Etzelmüller, Bernd Isaksen, Ketil Czekirda, Justyna Westermann, Sebastian Hilbich, Christin Hauck, Christian 2023-12-22 application/pdf https://doi.org/10.5194/tc-17-5477-2023 https://tc.copernicus.org/articles/17/5477/2023/ eng eng doi:10.5194/tc-17-5477-2023 https://tc.copernicus.org/articles/17/5477/2023/ eISSN: 1994-0424 Text 2023 ftcopernicus https://doi.org/10.5194/tc-17-5477-2023 2023-12-25T17:24:15Z With the EU-funded PACE (Permafrost and Climate in Europe) project at the turn of this century, several deep boreholes (100 m + ) were drilled in European mountain sites, including in mainland Norway, Svalbard and Sweden. During other projects from 2004 and the International Polar Year (IPY) period in 2006–2007, several additional boreholes were drilled in different sites in both Norway and Iceland, measuring temperatures along both altitudinal and latitudinal gradients. At most sites, multi-temporal geophysical soundings are available using electrical resistivity tomography (ERT). Here, we study the development of permafrost and ground temperatures in mainland Norway and Iceland based on these data sets. We document that permafrost in Norway and Iceland is warming at a high rate, including the development of taliks in both Norway and Iceland in response to global climate change during the last 20 years. At most sites, ground surface temperature (GST) is apparently increasing more strongly than surface air temperature (SAT). Changing snow conditions appear to be the most important factor for the higher GST rates. Modelling exercises also indicate that the talik development can be explained by both higher air temperatures and increasing snow depth. Text Iceland International Polar Year IPY permafrost Svalbard Copernicus Publications: E-Journals Norway Svalbard Talik ENVELOPE(146.601,146.601,59.667,59.667) The Cryosphere 17 12 5477 5497
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description With the EU-funded PACE (Permafrost and Climate in Europe) project at the turn of this century, several deep boreholes (100 m + ) were drilled in European mountain sites, including in mainland Norway, Svalbard and Sweden. During other projects from 2004 and the International Polar Year (IPY) period in 2006–2007, several additional boreholes were drilled in different sites in both Norway and Iceland, measuring temperatures along both altitudinal and latitudinal gradients. At most sites, multi-temporal geophysical soundings are available using electrical resistivity tomography (ERT). Here, we study the development of permafrost and ground temperatures in mainland Norway and Iceland based on these data sets. We document that permafrost in Norway and Iceland is warming at a high rate, including the development of taliks in both Norway and Iceland in response to global climate change during the last 20 years. At most sites, ground surface temperature (GST) is apparently increasing more strongly than surface air temperature (SAT). Changing snow conditions appear to be the most important factor for the higher GST rates. Modelling exercises also indicate that the talik development can be explained by both higher air temperatures and increasing snow depth.
format Text
author Etzelmüller, Bernd
Isaksen, Ketil
Czekirda, Justyna
Westermann, Sebastian
Hilbich, Christin
Hauck, Christian
spellingShingle Etzelmüller, Bernd
Isaksen, Ketil
Czekirda, Justyna
Westermann, Sebastian
Hilbich, Christin
Hauck, Christian
Rapid warming and degradation of mountain permafrost in Norway and Iceland
author_facet Etzelmüller, Bernd
Isaksen, Ketil
Czekirda, Justyna
Westermann, Sebastian
Hilbich, Christin
Hauck, Christian
author_sort Etzelmüller, Bernd
title Rapid warming and degradation of mountain permafrost in Norway and Iceland
title_short Rapid warming and degradation of mountain permafrost in Norway and Iceland
title_full Rapid warming and degradation of mountain permafrost in Norway and Iceland
title_fullStr Rapid warming and degradation of mountain permafrost in Norway and Iceland
title_full_unstemmed Rapid warming and degradation of mountain permafrost in Norway and Iceland
title_sort rapid warming and degradation of mountain permafrost in norway and iceland
publishDate 2023
url https://doi.org/10.5194/tc-17-5477-2023
https://tc.copernicus.org/articles/17/5477/2023/
long_lat ENVELOPE(146.601,146.601,59.667,59.667)
geographic Norway
Svalbard
Talik
geographic_facet Norway
Svalbard
Talik
genre Iceland
International Polar Year
IPY
permafrost
Svalbard
genre_facet Iceland
International Polar Year
IPY
permafrost
Svalbard
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-17-5477-2023
https://tc.copernicus.org/articles/17/5477/2023/
op_doi https://doi.org/10.5194/tc-17-5477-2023
container_title The Cryosphere
container_volume 17
container_issue 12
container_start_page 5477
op_container_end_page 5497
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