Twenty years of European mountain permafrost dynamics—the PACE legacy
This paper reviews and analyses the past 20 years of change and variability of European mountain permafrost in response to climate change based on time series of ground temperatures along a south–north transect of deep boreholes from Sierra Nevada in Spain (37°N) to Svalbard (78°N), established betw...
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Online Access: | https://doi.org/10.1088/1748-9326/abae9d https://doaj.org/article/f08dc695f72c4536a1866dee1eb1560b |
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ftdoajarticles:oai:doaj.org/article:f08dc695f72c4536a1866dee1eb1560b 2023-09-05T13:11:10+02:00 Twenty years of European mountain permafrost dynamics—the PACE legacy B Etzelmüller M Guglielmin C Hauck C Hilbich M Hoelzle K Isaksen J Noetzli M Oliva M Ramos 2020-01-01T00:00:00Z https://doi.org/10.1088/1748-9326/abae9d https://doaj.org/article/f08dc695f72c4536a1866dee1eb1560b EN eng IOP Publishing https://doi.org/10.1088/1748-9326/abae9d https://doaj.org/toc/1748-9326 doi:10.1088/1748-9326/abae9d 1748-9326 https://doaj.org/article/f08dc695f72c4536a1866dee1eb1560b Environmental Research Letters, Vol 15, Iss 10, p 104070 (2020) mountain permafrost PACE Europe monitoring climate change recent warming Environmental technology. Sanitary engineering TD1-1066 Environmental sciences GE1-350 Science Q Physics QC1-999 article 2020 ftdoajarticles https://doi.org/10.1088/1748-9326/abae9d 2023-08-13T00:37:16Z This paper reviews and analyses the past 20 years of change and variability of European mountain permafrost in response to climate change based on time series of ground temperatures along a south–north transect of deep boreholes from Sierra Nevada in Spain (37°N) to Svalbard (78°N), established between 1998 and 2000 during the EU-funded PACE (Permafrost and Climate in Europe) project. In Sierra Nevada (at the Veleta Peak), no permafrost is encountered. All other boreholes are drilled in permafrost. Results show that permafrost warmed at all sites down to depths of 50 m or more. The warming at a 20 m depth varied between 1.5 °C on Svalbard and 0.4 °C in the Alps. Warming rates tend to be less pronounced in the warm permafrost boreholes, which is partly due to latent heat effects at more ice-rich sites with ground temperatures close to 0 °C. At most sites, the air temperature at 2 m height showed a smaller increase than the near-ground-surface temperature, leading to an increase of surface offsets (SOs). The active layer thickness (ALT) increased at all sites between c. 10% and 200% with respect to the start of the study period, with the largest changes observed in the European Alps. Multi-temporal electrical resistivity tomography (ERT) carried out at six sites showed a decrease in electrical resistivity, independently supporting our conclusion of ground ice degradation and higher unfrozen water content. Article in Journal/Newspaper Active layer thickness Ice permafrost Svalbard Directory of Open Access Journals: DOAJ Articles Svalbard Environmental Research Letters 15 10 104070 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
mountain permafrost PACE Europe monitoring climate change recent warming Environmental technology. Sanitary engineering TD1-1066 Environmental sciences GE1-350 Science Q Physics QC1-999 |
spellingShingle |
mountain permafrost PACE Europe monitoring climate change recent warming Environmental technology. Sanitary engineering TD1-1066 Environmental sciences GE1-350 Science Q Physics QC1-999 B Etzelmüller M Guglielmin C Hauck C Hilbich M Hoelzle K Isaksen J Noetzli M Oliva M Ramos Twenty years of European mountain permafrost dynamics—the PACE legacy |
topic_facet |
mountain permafrost PACE Europe monitoring climate change recent warming Environmental technology. Sanitary engineering TD1-1066 Environmental sciences GE1-350 Science Q Physics QC1-999 |
description |
This paper reviews and analyses the past 20 years of change and variability of European mountain permafrost in response to climate change based on time series of ground temperatures along a south–north transect of deep boreholes from Sierra Nevada in Spain (37°N) to Svalbard (78°N), established between 1998 and 2000 during the EU-funded PACE (Permafrost and Climate in Europe) project. In Sierra Nevada (at the Veleta Peak), no permafrost is encountered. All other boreholes are drilled in permafrost. Results show that permafrost warmed at all sites down to depths of 50 m or more. The warming at a 20 m depth varied between 1.5 °C on Svalbard and 0.4 °C in the Alps. Warming rates tend to be less pronounced in the warm permafrost boreholes, which is partly due to latent heat effects at more ice-rich sites with ground temperatures close to 0 °C. At most sites, the air temperature at 2 m height showed a smaller increase than the near-ground-surface temperature, leading to an increase of surface offsets (SOs). The active layer thickness (ALT) increased at all sites between c. 10% and 200% with respect to the start of the study period, with the largest changes observed in the European Alps. Multi-temporal electrical resistivity tomography (ERT) carried out at six sites showed a decrease in electrical resistivity, independently supporting our conclusion of ground ice degradation and higher unfrozen water content. |
format |
Article in Journal/Newspaper |
author |
B Etzelmüller M Guglielmin C Hauck C Hilbich M Hoelzle K Isaksen J Noetzli M Oliva M Ramos |
author_facet |
B Etzelmüller M Guglielmin C Hauck C Hilbich M Hoelzle K Isaksen J Noetzli M Oliva M Ramos |
author_sort |
B Etzelmüller |
title |
Twenty years of European mountain permafrost dynamics—the PACE legacy |
title_short |
Twenty years of European mountain permafrost dynamics—the PACE legacy |
title_full |
Twenty years of European mountain permafrost dynamics—the PACE legacy |
title_fullStr |
Twenty years of European mountain permafrost dynamics—the PACE legacy |
title_full_unstemmed |
Twenty years of European mountain permafrost dynamics—the PACE legacy |
title_sort |
twenty years of european mountain permafrost dynamics—the pace legacy |
publisher |
IOP Publishing |
publishDate |
2020 |
url |
https://doi.org/10.1088/1748-9326/abae9d https://doaj.org/article/f08dc695f72c4536a1866dee1eb1560b |
geographic |
Svalbard |
geographic_facet |
Svalbard |
genre |
Active layer thickness Ice permafrost Svalbard |
genre_facet |
Active layer thickness Ice permafrost Svalbard |
op_source |
Environmental Research Letters, Vol 15, Iss 10, p 104070 (2020) |
op_relation |
https://doi.org/10.1088/1748-9326/abae9d https://doaj.org/toc/1748-9326 doi:10.1088/1748-9326/abae9d 1748-9326 https://doaj.org/article/f08dc695f72c4536a1866dee1eb1560b |
op_doi |
https://doi.org/10.1088/1748-9326/abae9d |
container_title |
Environmental Research Letters |
container_volume |
15 |
container_issue |
10 |
container_start_page |
104070 |
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1776198535508656128 |