Recent Advances in Mountain Permafrost Research

Knowledge of the thermal state of mountain permafrost has greatly increased since 2007 with the establishment of numerous new monitoring stations around the world. Data collected at these sites have pointed to longer‐term changes in ground temperatures, which seem to have increased during the last t...

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Published in:Permafrost and Periglacial Processes
Main Author: Bernd Etzelmüller
Format: Article in Journal/Newspaper
Language:unknown
Subjects:
Ice
Online Access:https://doi.org/10.1002/ppp.1772
id ftrepec:oai:RePEc:wly:perpro:v:24:y:2013:i:2:p:99-107
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spelling ftrepec:oai:RePEc:wly:perpro:v:24:y:2013:i:2:p:99-107 2023-05-15T16:37:00+02:00 Recent Advances in Mountain Permafrost Research Bernd Etzelmüller https://doi.org/10.1002/ppp.1772 unknown https://doi.org/10.1002/ppp.1772 article ftrepec https://doi.org/10.1002/ppp.1772 2020-12-04T13:31:25Z Knowledge of the thermal state of mountain permafrost has greatly increased since 2007 with the establishment of numerous new monitoring stations around the world. Data collected at these sites have pointed to longer‐term changes in ground temperatures, which seem to have increased during the last two to three decades in cold permafrost, while in ground close to 0°C the near‐surface ice content has restricted warming and similar trends are not apparent. Modelling of mountain permafrost has developed greatly, driven by general circulation models or gridded temperature maps, through both predictive methods and spatial equilibrium and transient approaches. The spatial resolution of climate parameters, which is normally much coarser than the spatial heterogeneity of alpine environments, presents a major problem for modelling studies. This is a fundamental challenge for future research. Copyright © 2013 John Wiley & Sons, Ltd. Article in Journal/Newspaper Ice permafrost RePEc (Research Papers in Economics) Permafrost and Periglacial Processes 24 2 99 107
institution Open Polar
collection RePEc (Research Papers in Economics)
op_collection_id ftrepec
language unknown
description Knowledge of the thermal state of mountain permafrost has greatly increased since 2007 with the establishment of numerous new monitoring stations around the world. Data collected at these sites have pointed to longer‐term changes in ground temperatures, which seem to have increased during the last two to three decades in cold permafrost, while in ground close to 0°C the near‐surface ice content has restricted warming and similar trends are not apparent. Modelling of mountain permafrost has developed greatly, driven by general circulation models or gridded temperature maps, through both predictive methods and spatial equilibrium and transient approaches. The spatial resolution of climate parameters, which is normally much coarser than the spatial heterogeneity of alpine environments, presents a major problem for modelling studies. This is a fundamental challenge for future research. Copyright © 2013 John Wiley & Sons, Ltd.
format Article in Journal/Newspaper
author Bernd Etzelmüller
spellingShingle Bernd Etzelmüller
Recent Advances in Mountain Permafrost Research
author_facet Bernd Etzelmüller
author_sort Bernd Etzelmüller
title Recent Advances in Mountain Permafrost Research
title_short Recent Advances in Mountain Permafrost Research
title_full Recent Advances in Mountain Permafrost Research
title_fullStr Recent Advances in Mountain Permafrost Research
title_full_unstemmed Recent Advances in Mountain Permafrost Research
title_sort recent advances in mountain permafrost research
url https://doi.org/10.1002/ppp.1772
genre Ice
permafrost
genre_facet Ice
permafrost
op_relation https://doi.org/10.1002/ppp.1772
op_doi https://doi.org/10.1002/ppp.1772
container_title Permafrost and Periglacial Processes
container_volume 24
container_issue 2
container_start_page 99
op_container_end_page 107
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