Projected changes of snow conditions and avalanche activity in a warming climate: the French Alps over the 2020-2050 and 2070-2100 periods

[Departement_IRSTEA]Eaux [TR1_IRSTEA]RIVAGE [Departement_IRSTEA]Eaux [TR1_IRSTEA]RIVAGE International audience Projecting changes in snow cover due to climate warming is important for many societal issues, including the adaptation of avalanche risk mitigation strategies. Efficient modelling of futur...

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Published in:The Cryosphere
Main Authors: Castebrunet, H., Eckert, N., Giraud, G., Durand, Y., Morin, Soizic
Other Authors: Laboratoire de Génie Civil et d'Ingénierie Environnementale (LGCIE), Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-Institut National des Sciences Appliquées de Lyon (INSA Lyon), Université de Lyon-Institut National des Sciences Appliquées (INSA)-Institut National des Sciences Appliquées (INSA), Erosion torrentielle neige et avalanches (UR ETGR (ETNA)), Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA), Centre national de recherches météorologiques (CNRM), Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2014
Subjects:
Online Access:https://hal.science/hal-01122258
https://hal.science/hal-01122258/document
https://hal.science/hal-01122258/file/gr2014-pub00043710.pdf
https://doi.org/10.5194/tc-8-1673-2014
id ftinsu:oai:HAL:hal-01122258v1
record_format openpolar
institution Open Polar
collection Institut national des sciences de l'Univers: HAL-INSU
op_collection_id ftinsu
language English
topic CLIMATIC CHANGE
AVALANCHES
METEOROLOGY
CHUTE DE NEIGE
ESTIMATION
CHANGEMENT CLIMATIQUE
AVALANCHE
METEOROLOGIE
[SDE]Environmental Sciences
spellingShingle CLIMATIC CHANGE
AVALANCHES
METEOROLOGY
CHUTE DE NEIGE
ESTIMATION
CHANGEMENT CLIMATIQUE
AVALANCHE
METEOROLOGIE
[SDE]Environmental Sciences
Castebrunet, H.
Eckert, N.
Giraud, G.
Durand, Y.
Morin, Soizic
Projected changes of snow conditions and avalanche activity in a warming climate: the French Alps over the 2020-2050 and 2070-2100 periods
topic_facet CLIMATIC CHANGE
AVALANCHES
METEOROLOGY
CHUTE DE NEIGE
ESTIMATION
CHANGEMENT CLIMATIQUE
AVALANCHE
METEOROLOGIE
[SDE]Environmental Sciences
description [Departement_IRSTEA]Eaux [TR1_IRSTEA]RIVAGE [Departement_IRSTEA]Eaux [TR1_IRSTEA]RIVAGE International audience Projecting changes in snow cover due to climate warming is important for many societal issues, including the adaptation of avalanche risk mitigation strategies. Efficient modelling of future snow cover requires high resolution to properly resolve the topography. Here, we introduce results obtained through statistical downscaling techniques allowing simulations of future snowpack conditions including mechanical stability estimates for the mid and late 21st century in the French Alps under three climate change scenarios. Refined statistical descriptions of snowpack characteristics are provided in comparison to a 1960-1990 reference period, including latitudinal, altitudinal and seasonal gradients. These results are then used to feed a statistical model relating avalanche activity to snow and meteorological conditions, so as to produce the first projection on annual/seasonal timescales of future natural avalanche activity based on past observations. The resulting statistical indicators are fundamental for the mountain economy in terms of anticipation of changes. Whereas precipitation is expected to remain quite stationary, temperature increase interacting with topography will constrain the evolution of snow-related variables on all considered spatio-temporal scales and will, in particular, lead to a reduction of the dry snowpack and an increase of the wet snowpack. Overall, compared to the reference period, changes are strong for the end of the 21st century, but already significant for the mid century. Changes in winter are less important than in spring, but wet-snow conditions are projected to appear at high elevations earlier in the season. At the same altitude, the southern French Alps will not be significantly more affected than the northern French Alps, which means that the snowpack will be preserved for longer in the southern massifs which are higher on average. Regarding avalanche activity, a ...
author2 Laboratoire de Génie Civil et d'Ingénierie Environnementale (LGCIE)
Université Claude Bernard Lyon 1 (UCBL)
Université de Lyon-Université de Lyon-Institut National des Sciences Appliquées de Lyon (INSA Lyon)
Université de Lyon-Institut National des Sciences Appliquées (INSA)-Institut National des Sciences Appliquées (INSA)
Erosion torrentielle neige et avalanches (UR ETGR (ETNA))
Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)
Centre national de recherches météorologiques (CNRM)
Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP)
Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3)
Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3)
Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS)
format Article in Journal/Newspaper
author Castebrunet, H.
Eckert, N.
Giraud, G.
Durand, Y.
Morin, Soizic
author_facet Castebrunet, H.
Eckert, N.
Giraud, G.
Durand, Y.
Morin, Soizic
author_sort Castebrunet, H.
title Projected changes of snow conditions and avalanche activity in a warming climate: the French Alps over the 2020-2050 and 2070-2100 periods
title_short Projected changes of snow conditions and avalanche activity in a warming climate: the French Alps over the 2020-2050 and 2070-2100 periods
title_full Projected changes of snow conditions and avalanche activity in a warming climate: the French Alps over the 2020-2050 and 2070-2100 periods
title_fullStr Projected changes of snow conditions and avalanche activity in a warming climate: the French Alps over the 2020-2050 and 2070-2100 periods
title_full_unstemmed Projected changes of snow conditions and avalanche activity in a warming climate: the French Alps over the 2020-2050 and 2070-2100 periods
title_sort projected changes of snow conditions and avalanche activity in a warming climate: the french alps over the 2020-2050 and 2070-2100 periods
publisher HAL CCSD
publishDate 2014
url https://hal.science/hal-01122258
https://hal.science/hal-01122258/document
https://hal.science/hal-01122258/file/gr2014-pub00043710.pdf
https://doi.org/10.5194/tc-8-1673-2014
genre The Cryosphere
genre_facet The Cryosphere
op_source ISSN: 1994-0424
EISSN: 1994-0416
The Cryosphere
https://hal.science/hal-01122258
The Cryosphere, 2014, 8 (5), pp.1673-1697. ⟨10.5194/tc-8-1673-2014⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.5194/tc-8-1673-2014
hal-01122258
https://hal.science/hal-01122258
https://hal.science/hal-01122258/document
https://hal.science/hal-01122258/file/gr2014-pub00043710.pdf
doi:10.5194/tc-8-1673-2014
IRSTEA: PUB00043710
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.5194/tc-8-1673-2014
container_title The Cryosphere
container_volume 8
container_issue 5
container_start_page 1673
op_container_end_page 1697
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spelling ftinsu:oai:HAL:hal-01122258v1 2024-04-14T08:20:22+00:00 Projected changes of snow conditions and avalanche activity in a warming climate: the French Alps over the 2020-2050 and 2070-2100 periods Castebrunet, H. Eckert, N. Giraud, G. Durand, Y. Morin, Soizic Laboratoire de Génie Civil et d'Ingénierie Environnementale (LGCIE) Université Claude Bernard Lyon 1 (UCBL) Université de Lyon-Université de Lyon-Institut National des Sciences Appliquées de Lyon (INSA Lyon) Université de Lyon-Institut National des Sciences Appliquées (INSA)-Institut National des Sciences Appliquées (INSA) Erosion torrentielle neige et avalanches (UR ETGR (ETNA)) Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA) Centre national de recherches météorologiques (CNRM) Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP) Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS) 2014 https://hal.science/hal-01122258 https://hal.science/hal-01122258/document https://hal.science/hal-01122258/file/gr2014-pub00043710.pdf https://doi.org/10.5194/tc-8-1673-2014 en eng HAL CCSD Copernicus info:eu-repo/semantics/altIdentifier/doi/10.5194/tc-8-1673-2014 hal-01122258 https://hal.science/hal-01122258 https://hal.science/hal-01122258/document https://hal.science/hal-01122258/file/gr2014-pub00043710.pdf doi:10.5194/tc-8-1673-2014 IRSTEA: PUB00043710 info:eu-repo/semantics/OpenAccess ISSN: 1994-0424 EISSN: 1994-0416 The Cryosphere https://hal.science/hal-01122258 The Cryosphere, 2014, 8 (5), pp.1673-1697. ⟨10.5194/tc-8-1673-2014⟩ CLIMATIC CHANGE AVALANCHES METEOROLOGY CHUTE DE NEIGE ESTIMATION CHANGEMENT CLIMATIQUE AVALANCHE METEOROLOGIE [SDE]Environmental Sciences info:eu-repo/semantics/article Journal articles 2014 ftinsu https://doi.org/10.5194/tc-8-1673-2014 2024-03-21T17:24:46Z [Departement_IRSTEA]Eaux [TR1_IRSTEA]RIVAGE [Departement_IRSTEA]Eaux [TR1_IRSTEA]RIVAGE International audience Projecting changes in snow cover due to climate warming is important for many societal issues, including the adaptation of avalanche risk mitigation strategies. Efficient modelling of future snow cover requires high resolution to properly resolve the topography. Here, we introduce results obtained through statistical downscaling techniques allowing simulations of future snowpack conditions including mechanical stability estimates for the mid and late 21st century in the French Alps under three climate change scenarios. Refined statistical descriptions of snowpack characteristics are provided in comparison to a 1960-1990 reference period, including latitudinal, altitudinal and seasonal gradients. These results are then used to feed a statistical model relating avalanche activity to snow and meteorological conditions, so as to produce the first projection on annual/seasonal timescales of future natural avalanche activity based on past observations. The resulting statistical indicators are fundamental for the mountain economy in terms of anticipation of changes. Whereas precipitation is expected to remain quite stationary, temperature increase interacting with topography will constrain the evolution of snow-related variables on all considered spatio-temporal scales and will, in particular, lead to a reduction of the dry snowpack and an increase of the wet snowpack. Overall, compared to the reference period, changes are strong for the end of the 21st century, but already significant for the mid century. Changes in winter are less important than in spring, but wet-snow conditions are projected to appear at high elevations earlier in the season. At the same altitude, the southern French Alps will not be significantly more affected than the northern French Alps, which means that the snowpack will be preserved for longer in the southern massifs which are higher on average. Regarding avalanche activity, a ... Article in Journal/Newspaper The Cryosphere Institut national des sciences de l'Univers: HAL-INSU The Cryosphere 8 5 1673 1697