Modeling the temperature evolution of Svalbard permafrost during the 20th and 21st century
Variations in ground thermal conditions in Svalbard were studied based on measurements and modelling. Ground temperature data from boreholes were used to calibrate a transient heat flow model describing depth and time variations in temperatures. The model was subsequently forced with historical surf...
Published in: | The Cryosphere |
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Main Authors: | , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Copernicus Publications
2011
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Subjects: | |
Online Access: | https://doi.org/10.5194/tc-5-67-2011 http://www.the-cryosphere.net/5/67/2011/tc-5-67-2011.pdf https://doaj.org/article/ef69b3f9ddb940e193fdbaf93ef169fb |
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author | B. Etzelmüller T. V. Schuler K. Isaksen H. H. Christiansen H. Farbrot R. Benestad |
author_facet | B. Etzelmüller T. V. Schuler K. Isaksen H. H. Christiansen H. Farbrot R. Benestad |
author_sort | B. Etzelmüller |
collection | Unknown |
container_issue | 1 |
container_start_page | 67 |
container_title | The Cryosphere |
container_volume | 5 |
description | Variations in ground thermal conditions in Svalbard were studied based on measurements and modelling. Ground temperature data from boreholes were used to calibrate a transient heat flow model describing depth and time variations in temperatures. The model was subsequently forced with historical surface air temperature records and possible future temperatures downscaled from multiple global climate models. We discuss ground temperature development since the early 20th century, and the thermal responses in relation to ground characteristics and snow cover. The modelled ground temperatures show a gradual increase between 1912 and 2010, by about 1.5 °C to 2 °C at 20 m depth. The active layer thickness (ALT) is modelled to have increased slightly, with the rate of increase depending on water content of the near-surface layers. The used scenario runs predict a significant increase in ground temperatures and an increase of ALT depending on soil characteristics. |
format | Article in Journal/Newspaper |
genre | Active layer thickness permafrost Svalbard The Cryosphere |
genre_facet | Active layer thickness permafrost Svalbard The Cryosphere |
geographic | Svalbard |
geographic_facet | Svalbard |
id | fttriple:oai:gotriple.eu:oai:doaj.org/article:ef69b3f9ddb940e193fdbaf93ef169fb |
institution | Open Polar |
language | English |
op_collection_id | fttriple |
op_container_end_page | 79 |
op_doi | https://doi.org/10.5194/tc-5-67-2011 |
op_relation | doi:10.5194/tc-5-67-2011 1994-0416 1994-0424 http://www.the-cryosphere.net/5/67/2011/tc-5-67-2011.pdf https://doaj.org/article/ef69b3f9ddb940e193fdbaf93ef169fb |
op_rights | undefined |
op_source | The Cryosphere, Vol 5, Iss 1, Pp 67-79 (2011) |
publishDate | 2011 |
publisher | Copernicus Publications |
record_format | openpolar |
spelling | fttriple:oai:gotriple.eu:oai:doaj.org/article:ef69b3f9ddb940e193fdbaf93ef169fb 2025-01-16T18:35:36+00:00 Modeling the temperature evolution of Svalbard permafrost during the 20th and 21st century B. Etzelmüller T. V. Schuler K. Isaksen H. H. Christiansen H. Farbrot R. Benestad 2011-02-01 https://doi.org/10.5194/tc-5-67-2011 http://www.the-cryosphere.net/5/67/2011/tc-5-67-2011.pdf https://doaj.org/article/ef69b3f9ddb940e193fdbaf93ef169fb en eng Copernicus Publications doi:10.5194/tc-5-67-2011 1994-0416 1994-0424 http://www.the-cryosphere.net/5/67/2011/tc-5-67-2011.pdf https://doaj.org/article/ef69b3f9ddb940e193fdbaf93ef169fb undefined The Cryosphere, Vol 5, Iss 1, Pp 67-79 (2011) geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2011 fttriple https://doi.org/10.5194/tc-5-67-2011 2023-01-22T18:58:33Z Variations in ground thermal conditions in Svalbard were studied based on measurements and modelling. Ground temperature data from boreholes were used to calibrate a transient heat flow model describing depth and time variations in temperatures. The model was subsequently forced with historical surface air temperature records and possible future temperatures downscaled from multiple global climate models. We discuss ground temperature development since the early 20th century, and the thermal responses in relation to ground characteristics and snow cover. The modelled ground temperatures show a gradual increase between 1912 and 2010, by about 1.5 °C to 2 °C at 20 m depth. The active layer thickness (ALT) is modelled to have increased slightly, with the rate of increase depending on water content of the near-surface layers. The used scenario runs predict a significant increase in ground temperatures and an increase of ALT depending on soil characteristics. Article in Journal/Newspaper Active layer thickness permafrost Svalbard The Cryosphere Unknown Svalbard The Cryosphere 5 1 67 79 |
spellingShingle | geo envir B. Etzelmüller T. V. Schuler K. Isaksen H. H. Christiansen H. Farbrot R. Benestad Modeling the temperature evolution of Svalbard permafrost during the 20th and 21st century |
title | Modeling the temperature evolution of Svalbard permafrost during the 20th and 21st century |
title_full | Modeling the temperature evolution of Svalbard permafrost during the 20th and 21st century |
title_fullStr | Modeling the temperature evolution of Svalbard permafrost during the 20th and 21st century |
title_full_unstemmed | Modeling the temperature evolution of Svalbard permafrost during the 20th and 21st century |
title_short | Modeling the temperature evolution of Svalbard permafrost during the 20th and 21st century |
title_sort | modeling the temperature evolution of svalbard permafrost during the 20th and 21st century |
topic | geo envir |
topic_facet | geo envir |
url | https://doi.org/10.5194/tc-5-67-2011 http://www.the-cryosphere.net/5/67/2011/tc-5-67-2011.pdf https://doaj.org/article/ef69b3f9ddb940e193fdbaf93ef169fb |