Evaluation du risque de déstabilisation des infrastructures de haute montagne engendré par le réchauffement climatique dans les Alpes françaises

Due to ongoing global warming, high alpine environments are affected by significant changes, such as glacial retreat and permafrost warming, which can trigger mass movements in rock slopes or superficial deposits. These processes generate a risk of direct destabilisation for high mountain infrastruc...

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Bibliographic Details
Published in:Revue de géographie alpine
Main Authors: Pierre-Allain Duvillard, Ludovic Ravanel, Philip Deline
Format: Article in Journal/Newspaper
Language:English
French
Published: Institut de Géographie Alpine 2015
Subjects:
G
Ice
Online Access:https://doi.org/10.4000/rga.2816
https://doaj.org/article/b8a6336f8fe14200a9d0db0a3384fd05
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spelling ftdoajarticles:oai:doaj.org/article:b8a6336f8fe14200a9d0db0a3384fd05 2023-05-15T16:37:11+02:00 Evaluation du risque de déstabilisation des infrastructures de haute montagne engendré par le réchauffement climatique dans les Alpes françaises Pierre-Allain Duvillard Ludovic Ravanel Philip Deline 2015-09-01T00:00:00Z https://doi.org/10.4000/rga.2816 https://doaj.org/article/b8a6336f8fe14200a9d0db0a3384fd05 EN FR eng fre Institut de Géographie Alpine http://journals.openedition.org/rga/2816 https://doaj.org/toc/0035-1121 https://doaj.org/toc/1760-7426 0035-1121 1760-7426 doi:10.4000/rga.2816 https://doaj.org/article/b8a6336f8fe14200a9d0db0a3384fd05 Revue de Géographie Alpine, Vol 103, Iss 2 (2015) high mountain infrastructure risk index permafrost degradation glacier shrinkage French Alps Geography. Anthropology. Recreation G Physical geography GB3-5030 article 2015 ftdoajarticles https://doi.org/10.4000/rga.2816 2022-12-31T07:04:14Z Due to ongoing global warming, high alpine environments are affected by significant changes, such as glacial retreat and permafrost warming, which can trigger mass movements in rock slopes or superficial deposits. These processes generate a risk of direct destabilisation for high mountain infrastructures (huts, cable cars, etc.). To help prevent such risks, an inventory of all the high mountain infrastructures in the French Alps was carried out using a Geographic Information System. This combined several data layers, including the Alpine Permafrost Index Map and glacier inventories since the end of the Little Ice Age. 1,769 infrastructures were identified in areas probably characterised by permafrost and/or possibly affected by glacier shrinkage. An index of destabilisation risk was constructed to identify and rank infrastructures at risk. This theoretical risk index includes a characterisation of hazards and a diagnosis of vulnerability. 10 % of the infrastructures were characterised by a high risk of destabilisation. Article in Journal/Newspaper Ice permafrost Directory of Open Access Journals: DOAJ Articles Revue de géographie alpine 103-2
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
French
topic high mountain infrastructure
risk index
permafrost degradation
glacier shrinkage
French Alps
Geography. Anthropology. Recreation
G
Physical geography
GB3-5030
spellingShingle high mountain infrastructure
risk index
permafrost degradation
glacier shrinkage
French Alps
Geography. Anthropology. Recreation
G
Physical geography
GB3-5030
Pierre-Allain Duvillard
Ludovic Ravanel
Philip Deline
Evaluation du risque de déstabilisation des infrastructures de haute montagne engendré par le réchauffement climatique dans les Alpes françaises
topic_facet high mountain infrastructure
risk index
permafrost degradation
glacier shrinkage
French Alps
Geography. Anthropology. Recreation
G
Physical geography
GB3-5030
description Due to ongoing global warming, high alpine environments are affected by significant changes, such as glacial retreat and permafrost warming, which can trigger mass movements in rock slopes or superficial deposits. These processes generate a risk of direct destabilisation for high mountain infrastructures (huts, cable cars, etc.). To help prevent such risks, an inventory of all the high mountain infrastructures in the French Alps was carried out using a Geographic Information System. This combined several data layers, including the Alpine Permafrost Index Map and glacier inventories since the end of the Little Ice Age. 1,769 infrastructures were identified in areas probably characterised by permafrost and/or possibly affected by glacier shrinkage. An index of destabilisation risk was constructed to identify and rank infrastructures at risk. This theoretical risk index includes a characterisation of hazards and a diagnosis of vulnerability. 10 % of the infrastructures were characterised by a high risk of destabilisation.
format Article in Journal/Newspaper
author Pierre-Allain Duvillard
Ludovic Ravanel
Philip Deline
author_facet Pierre-Allain Duvillard
Ludovic Ravanel
Philip Deline
author_sort Pierre-Allain Duvillard
title Evaluation du risque de déstabilisation des infrastructures de haute montagne engendré par le réchauffement climatique dans les Alpes françaises
title_short Evaluation du risque de déstabilisation des infrastructures de haute montagne engendré par le réchauffement climatique dans les Alpes françaises
title_full Evaluation du risque de déstabilisation des infrastructures de haute montagne engendré par le réchauffement climatique dans les Alpes françaises
title_fullStr Evaluation du risque de déstabilisation des infrastructures de haute montagne engendré par le réchauffement climatique dans les Alpes françaises
title_full_unstemmed Evaluation du risque de déstabilisation des infrastructures de haute montagne engendré par le réchauffement climatique dans les Alpes françaises
title_sort evaluation du risque de déstabilisation des infrastructures de haute montagne engendré par le réchauffement climatique dans les alpes françaises
publisher Institut de Géographie Alpine
publishDate 2015
url https://doi.org/10.4000/rga.2816
https://doaj.org/article/b8a6336f8fe14200a9d0db0a3384fd05
genre Ice
permafrost
genre_facet Ice
permafrost
op_source Revue de Géographie Alpine, Vol 103, Iss 2 (2015)
op_relation http://journals.openedition.org/rga/2816
https://doaj.org/toc/0035-1121
https://doaj.org/toc/1760-7426
0035-1121
1760-7426
doi:10.4000/rga.2816
https://doaj.org/article/b8a6336f8fe14200a9d0db0a3384fd05
op_doi https://doi.org/10.4000/rga.2816
container_title Revue de géographie alpine
container_issue 103-2
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