Snow control on active layer and permafrost in steep alpine rock walls (Aiguille du Midi, 3842 m a.s.l, Mont Blanc massif).
International audience Processes that control climate-dependent rockfall from permafrost-affected rock slopes are still poorly understood.In this study, we present the results of a Wireless Sensor Network, integrated within the Swiss project PermaSenseand developed in 2012, to measure rock temperatu...
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fttriple:oai:gotriple.eu:4kqitPe9UOXJUWOLSHTAq 2023-05-15T17:57:19+02:00 Snow control on active layer and permafrost in steep alpine rock walls (Aiguille du Midi, 3842 m a.s.l, Mont Blanc massif). Magnin, Florence Westermann, Sebastien Pogliotti, Paolo Ravanel, Ludovic Deline, Philip Environnements, Dynamiques et Territoires de la Montagne (EDYTEM) Centre National de la Recherche Scientifique (CNRS)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry ) Department of Geosciences Oslo Faculty of Mathematics and Natural Sciences Oslo University of Oslo (UiO)-University of Oslo (UiO) ARPA Valle d'Aosta (Aosta Valley Regional Environmental Protection Agency) Aosta Valley Regional Environmental Protection Agency (ARPA) European Geosciences Union Vienne, Austria 2016-04-17 https://hal-sde.archives-ouvertes.fr/hal-01788521 en eng HAL CCSD hal-01788521 10670/1.jwz2x1 hal-01781299 10670/1.u1cadt https://hal-sde.archives-ouvertes.fr/hal-01788521 undefined Hyper Article en Ligne - Sciences de l'Homme et de la Société EGU 2016 EGU 2016, European Geosciences Union, Apr 2016, Vienne, Austria geo envir Conference Output https://vocabularies.coar-repositories.org/resource_types/c_c94f/ 2016 fttriple 2023-01-22T17:39:48Z International audience Processes that control climate-dependent rockfall from permafrost-affected rock slopes are still poorly understood.In this study, we present the results of a Wireless Sensor Network, integrated within the Swiss project PermaSenseand developed in 2012, to measure rock temperature and geotechnical parameters in the steep rockwalls of theAiguille du Midi (AdM, 3842 m a.s.l., Mont Blanc massif, France). Accessible year round by cable car, the AdMcomprises two main peaks: (i) the Piton Nord with the cable car arrival station, where 4 crack-meters are placed onfour major fractures, and (ii) the Piton Central with many touristic infrastructure, equipped with three 10-m-deepboreholes with 15 temperatures sensors since 2009, and where 2 crack-meters are installed along a major fracture.Three major kinematic regimes are observed: (i) opening of clefts when the rock temperature becomes positive,followed by closing during the cold period, (ii) summer opening continued by a winter opening, and (iii) closingduring the warm period followed by opening in winter. Other/Unknown Material permafrost Unknown Mont Blanc ENVELOPE(69.468,69.468,-49.461,-49.461) Piton ENVELOPE(141.596,141.596,-66.777,-66.777) Piton Central ENVELOPE(69.543,69.543,-49.591,-49.591) |
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English |
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geo envir |
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geo envir Magnin, Florence Westermann, Sebastien Pogliotti, Paolo Ravanel, Ludovic Deline, Philip Snow control on active layer and permafrost in steep alpine rock walls (Aiguille du Midi, 3842 m a.s.l, Mont Blanc massif). |
topic_facet |
geo envir |
description |
International audience Processes that control climate-dependent rockfall from permafrost-affected rock slopes are still poorly understood.In this study, we present the results of a Wireless Sensor Network, integrated within the Swiss project PermaSenseand developed in 2012, to measure rock temperature and geotechnical parameters in the steep rockwalls of theAiguille du Midi (AdM, 3842 m a.s.l., Mont Blanc massif, France). Accessible year round by cable car, the AdMcomprises two main peaks: (i) the Piton Nord with the cable car arrival station, where 4 crack-meters are placed onfour major fractures, and (ii) the Piton Central with many touristic infrastructure, equipped with three 10-m-deepboreholes with 15 temperatures sensors since 2009, and where 2 crack-meters are installed along a major fracture.Three major kinematic regimes are observed: (i) opening of clefts when the rock temperature becomes positive,followed by closing during the cold period, (ii) summer opening continued by a winter opening, and (iii) closingduring the warm period followed by opening in winter. |
author2 |
Environnements, Dynamiques et Territoires de la Montagne (EDYTEM) Centre National de la Recherche Scientifique (CNRS)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry ) Department of Geosciences Oslo Faculty of Mathematics and Natural Sciences Oslo University of Oslo (UiO)-University of Oslo (UiO) ARPA Valle d'Aosta (Aosta Valley Regional Environmental Protection Agency) Aosta Valley Regional Environmental Protection Agency (ARPA) European Geosciences Union |
format |
Other/Unknown Material |
author |
Magnin, Florence Westermann, Sebastien Pogliotti, Paolo Ravanel, Ludovic Deline, Philip |
author_facet |
Magnin, Florence Westermann, Sebastien Pogliotti, Paolo Ravanel, Ludovic Deline, Philip |
author_sort |
Magnin, Florence |
title |
Snow control on active layer and permafrost in steep alpine rock walls (Aiguille du Midi, 3842 m a.s.l, Mont Blanc massif). |
title_short |
Snow control on active layer and permafrost in steep alpine rock walls (Aiguille du Midi, 3842 m a.s.l, Mont Blanc massif). |
title_full |
Snow control on active layer and permafrost in steep alpine rock walls (Aiguille du Midi, 3842 m a.s.l, Mont Blanc massif). |
title_fullStr |
Snow control on active layer and permafrost in steep alpine rock walls (Aiguille du Midi, 3842 m a.s.l, Mont Blanc massif). |
title_full_unstemmed |
Snow control on active layer and permafrost in steep alpine rock walls (Aiguille du Midi, 3842 m a.s.l, Mont Blanc massif). |
title_sort |
snow control on active layer and permafrost in steep alpine rock walls (aiguille du midi, 3842 m a.s.l, mont blanc massif). |
publisher |
HAL CCSD |
publishDate |
2016 |
url |
https://hal-sde.archives-ouvertes.fr/hal-01788521 |
op_coverage |
Vienne, Austria |
long_lat |
ENVELOPE(69.468,69.468,-49.461,-49.461) ENVELOPE(141.596,141.596,-66.777,-66.777) ENVELOPE(69.543,69.543,-49.591,-49.591) |
geographic |
Mont Blanc Piton Piton Central |
geographic_facet |
Mont Blanc Piton Piton Central |
genre |
permafrost |
genre_facet |
permafrost |
op_source |
Hyper Article en Ligne - Sciences de l'Homme et de la Société EGU 2016 EGU 2016, European Geosciences Union, Apr 2016, Vienne, Austria |
op_relation |
hal-01788521 10670/1.jwz2x1 hal-01781299 10670/1.u1cadt https://hal-sde.archives-ouvertes.fr/hal-01788521 |
op_rights |
undefined |
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1766165714888032256 |