New insights into the environmental factors controlling the ground thermal regime across the Northern Hemisphere : a comparison between permafrost and non-permafrost areas
The thermal state of permafrost affects Earth surface systems and human activity in the Arctic and has implications for global climate. Improved understanding of the local-scale variability in the global ground thermal regime is required to account for its sensitivity to changing climatic and geoeco...
Published in: | The Cryosphere |
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Main Authors: | , , , |
Other Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
COPERNICUS GESELLSCHAFT MBH
2019
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Subjects: | |
Online Access: | http://hdl.handle.net/10138/299882 |
_version_ | 1821845292306137088 |
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author | Karjalainen, Olli Luoto, Miska Aalto, Juha Hjort, Jan |
author2 | Helsinki Institute of Sustainability Science (HELSUS) Department of Geosciences and Geography BioGeoClimate Modelling Lab |
author_facet | Karjalainen, Olli Luoto, Miska Aalto, Juha Hjort, Jan |
author_sort | Karjalainen, Olli |
collection | HELDA – University of Helsinki Open Repository |
container_issue | 2 |
container_start_page | 693 |
container_title | The Cryosphere |
container_volume | 13 |
description | The thermal state of permafrost affects Earth surface systems and human activity in the Arctic and has implications for global climate. Improved understanding of the local-scale variability in the global ground thermal regime is required to account for its sensitivity to changing climatic and geoecological conditions. Here, we statistically related observations of mean annual ground temperature (MAGT) and active-layer thickness (ALT) to high-resolution (similar to 1 km(2)) geospatial data of climatic and local environmental conditions across the Northern Hemisphere. The aim was to characterize the relative importance of key environmental factors and the magnitude and shape of their effects on MAGT and ALT. The multivariate models fitted well to both response variables with average R-2 values being similar to 0.94 and 0.78. Corresponding predictive performances in terms of root-mean-square error were similar to 1.31 degrees C and 87 cm. Freezing (FDD) and thawing (TDD) degree days were key factors for MAGT inside and outside the permafrost domain with average effect sizes of 6.7 and 13.6 degrees C, respectively. Soil properties had marginal effects on MAGT (effect size = 0.4-0.7 degrees C). For ALT, rainfall (effect size = 181 cm) and solar radiation (161 cm) were most influential. Analysis of variable importance further underlined the dominance of climate for MAGT and highlighted the role of solar radiation for ALT. Most response shapes for MAGT Peer reviewed |
format | Article in Journal/Newspaper |
genre | Active layer thickness Arctic permafrost |
genre_facet | Active layer thickness Arctic permafrost |
geographic | Arctic |
geographic_facet | Arctic |
id | ftunivhelsihelda:oai:helda.helsinki.fi:10138/299882 |
institution | Open Polar |
language | English |
op_collection_id | ftunivhelsihelda |
op_container_end_page | 707 |
op_relation | 10.5194/tc-13-693-2019 Karjalainen , O , Luoto , M , Aalto , J & Hjort , J 2019 , ' New insights into the environmental factors controlling the ground thermal regime across the Northern Hemisphere : a comparison between permafrost and non-permafrost areas ' , Cryosphere , vol. 13 , no. 2 , pp. 693-707 . https://doi.org/10.5194/tc-13-693-2019 ORCID: /0000-0001-6203-5143/work/55060066 ORCID: /0000-0001-6819-4911/work/55063183 85062348531 c666c0cd-0e29-4a7e-9bf6-0e0121a6399f http://hdl.handle.net/10138/299882 000459979600002 |
op_rights | cc_by openAccess info:eu-repo/semantics/openAccess |
publishDate | 2019 |
publisher | COPERNICUS GESELLSCHAFT MBH |
record_format | openpolar |
spelling | ftunivhelsihelda:oai:helda.helsinki.fi:10138/299882 2025-01-16T18:35:09+00:00 New insights into the environmental factors controlling the ground thermal regime across the Northern Hemisphere : a comparison between permafrost and non-permafrost areas Karjalainen, Olli Luoto, Miska Aalto, Juha Hjort, Jan Helsinki Institute of Sustainability Science (HELSUS) Department of Geosciences and Geography BioGeoClimate Modelling Lab 2019-03-06T07:04:01Z 15 application/pdf http://hdl.handle.net/10138/299882 eng eng COPERNICUS GESELLSCHAFT MBH 10.5194/tc-13-693-2019 Karjalainen , O , Luoto , M , Aalto , J & Hjort , J 2019 , ' New insights into the environmental factors controlling the ground thermal regime across the Northern Hemisphere : a comparison between permafrost and non-permafrost areas ' , Cryosphere , vol. 13 , no. 2 , pp. 693-707 . https://doi.org/10.5194/tc-13-693-2019 ORCID: /0000-0001-6203-5143/work/55060066 ORCID: /0000-0001-6819-4911/work/55063183 85062348531 c666c0cd-0e29-4a7e-9bf6-0e0121a6399f http://hdl.handle.net/10138/299882 000459979600002 cc_by openAccess info:eu-repo/semantics/openAccess 1172 Environmental sciences ACTIVE-LAYER THICKNESS MOUNTAIN PERMAFROST SNOW COVER CLIMATE TEMPERATURES HEAT BASIN STATE Article publishedVersion 2019 ftunivhelsihelda 2023-12-14T00:07:06Z The thermal state of permafrost affects Earth surface systems and human activity in the Arctic and has implications for global climate. Improved understanding of the local-scale variability in the global ground thermal regime is required to account for its sensitivity to changing climatic and geoecological conditions. Here, we statistically related observations of mean annual ground temperature (MAGT) and active-layer thickness (ALT) to high-resolution (similar to 1 km(2)) geospatial data of climatic and local environmental conditions across the Northern Hemisphere. The aim was to characterize the relative importance of key environmental factors and the magnitude and shape of their effects on MAGT and ALT. The multivariate models fitted well to both response variables with average R-2 values being similar to 0.94 and 0.78. Corresponding predictive performances in terms of root-mean-square error were similar to 1.31 degrees C and 87 cm. Freezing (FDD) and thawing (TDD) degree days were key factors for MAGT inside and outside the permafrost domain with average effect sizes of 6.7 and 13.6 degrees C, respectively. Soil properties had marginal effects on MAGT (effect size = 0.4-0.7 degrees C). For ALT, rainfall (effect size = 181 cm) and solar radiation (161 cm) were most influential. Analysis of variable importance further underlined the dominance of climate for MAGT and highlighted the role of solar radiation for ALT. Most response shapes for MAGT Peer reviewed Article in Journal/Newspaper Active layer thickness Arctic permafrost HELDA – University of Helsinki Open Repository Arctic The Cryosphere 13 2 693 707 |
spellingShingle | 1172 Environmental sciences ACTIVE-LAYER THICKNESS MOUNTAIN PERMAFROST SNOW COVER CLIMATE TEMPERATURES HEAT BASIN STATE Karjalainen, Olli Luoto, Miska Aalto, Juha Hjort, Jan New insights into the environmental factors controlling the ground thermal regime across the Northern Hemisphere : a comparison between permafrost and non-permafrost areas |
title | New insights into the environmental factors controlling the ground thermal regime across the Northern Hemisphere : a comparison between permafrost and non-permafrost areas |
title_full | New insights into the environmental factors controlling the ground thermal regime across the Northern Hemisphere : a comparison between permafrost and non-permafrost areas |
title_fullStr | New insights into the environmental factors controlling the ground thermal regime across the Northern Hemisphere : a comparison between permafrost and non-permafrost areas |
title_full_unstemmed | New insights into the environmental factors controlling the ground thermal regime across the Northern Hemisphere : a comparison between permafrost and non-permafrost areas |
title_short | New insights into the environmental factors controlling the ground thermal regime across the Northern Hemisphere : a comparison between permafrost and non-permafrost areas |
title_sort | new insights into the environmental factors controlling the ground thermal regime across the northern hemisphere : a comparison between permafrost and non-permafrost areas |
topic | 1172 Environmental sciences ACTIVE-LAYER THICKNESS MOUNTAIN PERMAFROST SNOW COVER CLIMATE TEMPERATURES HEAT BASIN STATE |
topic_facet | 1172 Environmental sciences ACTIVE-LAYER THICKNESS MOUNTAIN PERMAFROST SNOW COVER CLIMATE TEMPERATURES HEAT BASIN STATE |
url | http://hdl.handle.net/10138/299882 |