Air warming trends linked to permafrost warming in the sub-Arctic catchment of Tarfala, Sweden

Recent ground temperature records from the 100-m-deep borehole near the Tarfala Research Station in northern Sweden reveal that permafrost is warming at a pace consistent with the rate of measured air temperature increase at the site. Here we investigate whether air temperature increase is the main...

Full description

Bibliographic Details
Published in:Polar Research
Main Authors: Romain Pannetier, Andrew Frampton
Format: Article in Journal/Newspaper
Language:English
Published: Norwegian Polar Institute 2016
Subjects:
geo
Online Access:https://doi.org/10.3402/polar.v35.28978
https://doaj.org/article/e0df8ab920034dfeb2b570677862cfc4
id fttriple:oai:gotriple.eu:oai:doaj.org/article:e0df8ab920034dfeb2b570677862cfc4
record_format openpolar
spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:e0df8ab920034dfeb2b570677862cfc4 2023-05-15T15:06:41+02:00 Air warming trends linked to permafrost warming in the sub-Arctic catchment of Tarfala, Sweden Romain Pannetier Andrew Frampton 2016-09-01 https://doi.org/10.3402/polar.v35.28978 https://doaj.org/article/e0df8ab920034dfeb2b570677862cfc4 en eng Norwegian Polar Institute 1751-8369 doi:10.3402/polar.v35.28978 https://doaj.org/article/e0df8ab920034dfeb2b570677862cfc4 undefined Polar Research, Vol 35, Iss 0, Pp 1-18 (2016) Permafrost warming ground PACE borehole numerical modelling climate change geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2016 fttriple https://doi.org/10.3402/polar.v35.28978 2023-01-22T19:27:58Z Recent ground temperature records from the 100-m-deep borehole near the Tarfala Research Station in northern Sweden reveal that permafrost is warming at a pace consistent with the rate of measured air temperature increase at the site. Here we investigate whether air temperature increase is the main driver of the observed change in the permafrost thermal regime using a non-isothermal hydrogeological numerical model for partially frozen ground. The local site is investigated with different ground surface temperature scenarios representing different integrated effects of surficial heat attenuation processes. Results indicate that despite a short-term sensitivity to heat attenuation processes including snow conditions, the main driver of change in the permafrost thermal regime during the past decade is warming air temperatures. Additionally, the approach used here is shown to be particularly pertinent for modelling warming trends, despite limited prior knowledge of site-specific conditions and geological properties. Understanding the main driving mechanisms of changing permafrost is useful for assessing the suitability of borehole temperature records as proxies for past environmental conditions as well as for modelling possible future climatic impacts. Article in Journal/Newspaper Arctic Climate change Northern Sweden permafrost Polar Research Tarfala Unknown Arctic Tarfala ENVELOPE(18.608,18.608,67.914,67.914) Polar Research 35 1 28978
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic Permafrost
warming ground
PACE borehole
numerical modelling
climate change
geo
envir
spellingShingle Permafrost
warming ground
PACE borehole
numerical modelling
climate change
geo
envir
Romain Pannetier
Andrew Frampton
Air warming trends linked to permafrost warming in the sub-Arctic catchment of Tarfala, Sweden
topic_facet Permafrost
warming ground
PACE borehole
numerical modelling
climate change
geo
envir
description Recent ground temperature records from the 100-m-deep borehole near the Tarfala Research Station in northern Sweden reveal that permafrost is warming at a pace consistent with the rate of measured air temperature increase at the site. Here we investigate whether air temperature increase is the main driver of the observed change in the permafrost thermal regime using a non-isothermal hydrogeological numerical model for partially frozen ground. The local site is investigated with different ground surface temperature scenarios representing different integrated effects of surficial heat attenuation processes. Results indicate that despite a short-term sensitivity to heat attenuation processes including snow conditions, the main driver of change in the permafrost thermal regime during the past decade is warming air temperatures. Additionally, the approach used here is shown to be particularly pertinent for modelling warming trends, despite limited prior knowledge of site-specific conditions and geological properties. Understanding the main driving mechanisms of changing permafrost is useful for assessing the suitability of borehole temperature records as proxies for past environmental conditions as well as for modelling possible future climatic impacts.
format Article in Journal/Newspaper
author Romain Pannetier
Andrew Frampton
author_facet Romain Pannetier
Andrew Frampton
author_sort Romain Pannetier
title Air warming trends linked to permafrost warming in the sub-Arctic catchment of Tarfala, Sweden
title_short Air warming trends linked to permafrost warming in the sub-Arctic catchment of Tarfala, Sweden
title_full Air warming trends linked to permafrost warming in the sub-Arctic catchment of Tarfala, Sweden
title_fullStr Air warming trends linked to permafrost warming in the sub-Arctic catchment of Tarfala, Sweden
title_full_unstemmed Air warming trends linked to permafrost warming in the sub-Arctic catchment of Tarfala, Sweden
title_sort air warming trends linked to permafrost warming in the sub-arctic catchment of tarfala, sweden
publisher Norwegian Polar Institute
publishDate 2016
url https://doi.org/10.3402/polar.v35.28978
https://doaj.org/article/e0df8ab920034dfeb2b570677862cfc4
long_lat ENVELOPE(18.608,18.608,67.914,67.914)
geographic Arctic
Tarfala
geographic_facet Arctic
Tarfala
genre Arctic
Climate change
Northern Sweden
permafrost
Polar Research
Tarfala
genre_facet Arctic
Climate change
Northern Sweden
permafrost
Polar Research
Tarfala
op_source Polar Research, Vol 35, Iss 0, Pp 1-18 (2016)
op_relation 1751-8369
doi:10.3402/polar.v35.28978
https://doaj.org/article/e0df8ab920034dfeb2b570677862cfc4
op_rights undefined
op_doi https://doi.org/10.3402/polar.v35.28978
container_title Polar Research
container_volume 35
container_issue 1
container_start_page 28978
_version_ 1766338244964777984