Modeling permafrost occurrence, glacier-bed topography and possible future lakes for assessing changing hazard conditions in cold mountain regions
International audience The rapid transformation of glacial into periglacial mountain landscapes under conditions of continued global warming can cause new and locally severe changes in hazard and risk conditions. A special focus must be on systematically increasing risks due to far-reaching flood wa...
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ftunivsavoie:oai:HAL:hal-03337508v1 2024-04-28T08:23:30+00:00 Modeling permafrost occurrence, glacier-bed topography and possible future lakes for assessing changing hazard conditions in cold mountain regions Haeberli, Wilfried Magnin, Florence Linsbauer, Andreas Environnements, Dynamiques et Territoires de Montagne (EDYTEM) Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS) Chamonix, France 2018-06-23 https://hal.science/hal-03337508 https://hal.science/hal-03337508/document https://hal.science/hal-03337508/file/EUCOP2018_Haeberli.pdf en eng HAL CCSD hal-03337508 https://hal.science/hal-03337508 https://hal.science/hal-03337508/document https://hal.science/hal-03337508/file/EUCOP2018_Haeberli.pdf info:eu-repo/semantics/OpenAccess 5th European Conference On Permafrost https://hal.science/hal-03337508 5th European Conference On Permafrost, Jun 2018, Chamonix, France global warming mountain permafrost glacier beds new lakes rock/ice avalanches natural hazards [SDE.ES]Environmental Sciences/Environment and Society [SDE]Environmental Sciences [SDE.MCG]Environmental Sciences/Global Changes info:eu-repo/semantics/conferenceObject Conference papers 2018 ftunivsavoie 2024-04-11T00:39:17Z International audience The rapid transformation of glacial into periglacial mountain landscapes under conditions of continued global warming can cause new and locally severe changes in hazard and risk conditions. A special focus must be on systematically increasing risks due to far-reaching flood waves or debris flows caused by rock/ice avalanches into new lakes at the foot of steep slopes with decreasing stability due to permafrost degradation and/or glacial de-buttressing. Modeling permafrost occurrence and glacier-bed topography provides important information for anticipating critical future situations. Conference Object Ice permafrost Université Savoie Mont Blanc: HAL |
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Open Polar |
collection |
Université Savoie Mont Blanc: HAL |
op_collection_id |
ftunivsavoie |
language |
English |
topic |
global warming mountain permafrost glacier beds new lakes rock/ice avalanches natural hazards [SDE.ES]Environmental Sciences/Environment and Society [SDE]Environmental Sciences [SDE.MCG]Environmental Sciences/Global Changes |
spellingShingle |
global warming mountain permafrost glacier beds new lakes rock/ice avalanches natural hazards [SDE.ES]Environmental Sciences/Environment and Society [SDE]Environmental Sciences [SDE.MCG]Environmental Sciences/Global Changes Haeberli, Wilfried Magnin, Florence Linsbauer, Andreas Modeling permafrost occurrence, glacier-bed topography and possible future lakes for assessing changing hazard conditions in cold mountain regions |
topic_facet |
global warming mountain permafrost glacier beds new lakes rock/ice avalanches natural hazards [SDE.ES]Environmental Sciences/Environment and Society [SDE]Environmental Sciences [SDE.MCG]Environmental Sciences/Global Changes |
description |
International audience The rapid transformation of glacial into periglacial mountain landscapes under conditions of continued global warming can cause new and locally severe changes in hazard and risk conditions. A special focus must be on systematically increasing risks due to far-reaching flood waves or debris flows caused by rock/ice avalanches into new lakes at the foot of steep slopes with decreasing stability due to permafrost degradation and/or glacial de-buttressing. Modeling permafrost occurrence and glacier-bed topography provides important information for anticipating critical future situations. |
author2 |
Environnements, Dynamiques et Territoires de Montagne (EDYTEM) Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS) |
format |
Conference Object |
author |
Haeberli, Wilfried Magnin, Florence Linsbauer, Andreas |
author_facet |
Haeberli, Wilfried Magnin, Florence Linsbauer, Andreas |
author_sort |
Haeberli, Wilfried |
title |
Modeling permafrost occurrence, glacier-bed topography and possible future lakes for assessing changing hazard conditions in cold mountain regions |
title_short |
Modeling permafrost occurrence, glacier-bed topography and possible future lakes for assessing changing hazard conditions in cold mountain regions |
title_full |
Modeling permafrost occurrence, glacier-bed topography and possible future lakes for assessing changing hazard conditions in cold mountain regions |
title_fullStr |
Modeling permafrost occurrence, glacier-bed topography and possible future lakes for assessing changing hazard conditions in cold mountain regions |
title_full_unstemmed |
Modeling permafrost occurrence, glacier-bed topography and possible future lakes for assessing changing hazard conditions in cold mountain regions |
title_sort |
modeling permafrost occurrence, glacier-bed topography and possible future lakes for assessing changing hazard conditions in cold mountain regions |
publisher |
HAL CCSD |
publishDate |
2018 |
url |
https://hal.science/hal-03337508 https://hal.science/hal-03337508/document https://hal.science/hal-03337508/file/EUCOP2018_Haeberli.pdf |
op_coverage |
Chamonix, France |
genre |
Ice permafrost |
genre_facet |
Ice permafrost |
op_source |
5th European Conference On Permafrost https://hal.science/hal-03337508 5th European Conference On Permafrost, Jun 2018, Chamonix, France |
op_relation |
hal-03337508 https://hal.science/hal-03337508 https://hal.science/hal-03337508/document https://hal.science/hal-03337508/file/EUCOP2018_Haeberli.pdf |
op_rights |
info:eu-repo/semantics/OpenAccess |
_version_ |
1797584412684058624 |