Limited impacts of global warming on rockfall activity at low elevations: Insights from two calcareous cliffs from the French Prealps

International audience In mountainous regions, global warming will likely affect the frequency and magnitude of geomorphic processes. This is also the case for rockfall, one of the most common mass movements on steep slopes. Rainfall, snowmelt, or freeze-thaw cycles are the main drivers of rockfall...

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Published in:Progress in Physical Geography: Earth and Environment
Main Authors: Mainieri, Robin, Eckert, Nicolas, Corona, Christophe, Lopez-Saez, Jerome, Stoffel, Markus, Bourrier, Franck
Other Authors: Ecosystèmes montagnards (UR EMGR), Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA), Laboratoire des EcoSystèmes et des Sociétés en Montagne (UR LESSEM), Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE), Institut des Géosciences de l’Environnement (IGE), Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP ), Université Grenoble Alpes (UGA), Erosion torrentielle neige et avalanches (UR ETGR (ETNA)), Institute for Environmental Sciences Geneva (ISE), Université de Genève = University of Geneva (UNIGE), Laboratoire de Géographie Physique et Environnementale (GEOLAB), Université Blaise Pascal - Clermont-Ferrand 2 (UBP)-Institut Sciences de l'Homme et de la Société (IR SHS UNILIM), Université de Limoges (UNILIM)-Université de Limoges (UNILIM)-Université Clermont Auvergne 2017-2020 (UCA 2017-2020 )-Centre National de la Recherche Scientifique (CNRS)-Université Clermont Auvergne (UCA), Dendrolab.ch Bern, Institute of Geological Sciences Bern, Universität Bern / University of Bern (UNIBE)-Universität Bern / University of Bern (UNIBE), ANR-15-IDEX-02
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2022
Subjects:
Online Access:https://hal.inrae.fr/hal-03790287
https://doi.org/10.1177/03091333221107624
id ftunivlimoges:oai:HAL:hal-03790287v1
record_format openpolar
institution Open Polar
collection Université de Limoges: HAL
op_collection_id ftunivlimoges
language English
topic Rockfall
tree-ring reconstruction
climate change
calcareous French Alps
[SDE.IE]Environmental Sciences/Environmental Engineering
[SDV]Life Sciences [q-bio]
spellingShingle Rockfall
tree-ring reconstruction
climate change
calcareous French Alps
[SDE.IE]Environmental Sciences/Environmental Engineering
[SDV]Life Sciences [q-bio]
Mainieri, Robin
Eckert, Nicolas
Corona, Christophe
Lopez-Saez, Jerome
Stoffel, Markus
Bourrier, Franck
Limited impacts of global warming on rockfall activity at low elevations: Insights from two calcareous cliffs from the French Prealps
topic_facet Rockfall
tree-ring reconstruction
climate change
calcareous French Alps
[SDE.IE]Environmental Sciences/Environmental Engineering
[SDV]Life Sciences [q-bio]
description International audience In mountainous regions, global warming will likely affect the frequency and magnitude of geomorphic processes. This is also the case for rockfall, one of the most common mass movements on steep slopes. Rainfall, snowmelt, or freeze-thaw cycles are the main drivers of rockfall activity, rockfall hazards are thus generally thought to become more relevant in a context of climate change. At high elevations, unequivocal relationships have been found between increased rockfall activity, permafrost thawing and global warming. By contrast, below the permafrost limit, studies are scarcer. They mostly rely on short or incomplete rockfall records, and have so far failed to identify climatically induced trends in rockfall records. Here, using a dendrogeomorphic approach, we develop two continuous 60-year long chronologies of rockfall activity in the Vercors and Diois massifs (French Alps); both sites are located clearly below the permafrost limit. Uncertainties related to the decreasing number of trees available back in time were quantified based on a detailed mapping of trees covering the slope across time. Significant multiple regression models with reconstructed rockfalls as predictors and local changes in climatic conditions since 1959 extracted from the SAFRAN reanalysis dataset as predictants were fitted to investigate the potential impacts of global warming on rockfall activity at both sites. In the Vercors massif, the strong increase in reconstructed rockfall can be ascribed to the recolonization of the forest stand and the over-representation of young trees; changes that are observed should not therefore be ascribed to climatic fluctuations. In the Diois massif, we identify annual precipitation totals and mean temperatures as statistically significant drivers of rockfall activity but no significant increasing trend was identified in the reconstruction. All in all, despite the stringency of our approach, we cannot therefore confirm that rockfall hazard will increase as a result of global ...
author2 Ecosystèmes montagnards (UR EMGR)
Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)
Laboratoire des EcoSystèmes et des Sociétés en Montagne (UR LESSEM)
Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)
Institut des Géosciences de l’Environnement (IGE)
Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )
Université Grenoble Alpes (UGA)
Erosion torrentielle neige et avalanches (UR ETGR (ETNA))
Institute for Environmental Sciences Geneva (ISE)
Université de Genève = University of Geneva (UNIGE)
Laboratoire de Géographie Physique et Environnementale (GEOLAB)
Université Blaise Pascal - Clermont-Ferrand 2 (UBP)-Institut Sciences de l'Homme et de la Société (IR SHS UNILIM)
Université de Limoges (UNILIM)-Université de Limoges (UNILIM)-Université Clermont Auvergne 2017-2020 (UCA 2017-2020 )-Centre National de la Recherche Scientifique (CNRS)-Université Clermont Auvergne (UCA)
Dendrolab.ch Bern
Institute of Geological Sciences Bern
Universität Bern / University of Bern (UNIBE)-Universität Bern / University of Bern (UNIBE)
ANR-15-IDEX-02
format Article in Journal/Newspaper
author Mainieri, Robin
Eckert, Nicolas
Corona, Christophe
Lopez-Saez, Jerome
Stoffel, Markus
Bourrier, Franck
author_facet Mainieri, Robin
Eckert, Nicolas
Corona, Christophe
Lopez-Saez, Jerome
Stoffel, Markus
Bourrier, Franck
author_sort Mainieri, Robin
title Limited impacts of global warming on rockfall activity at low elevations: Insights from two calcareous cliffs from the French Prealps
title_short Limited impacts of global warming on rockfall activity at low elevations: Insights from two calcareous cliffs from the French Prealps
title_full Limited impacts of global warming on rockfall activity at low elevations: Insights from two calcareous cliffs from the French Prealps
title_fullStr Limited impacts of global warming on rockfall activity at low elevations: Insights from two calcareous cliffs from the French Prealps
title_full_unstemmed Limited impacts of global warming on rockfall activity at low elevations: Insights from two calcareous cliffs from the French Prealps
title_sort limited impacts of global warming on rockfall activity at low elevations: insights from two calcareous cliffs from the french prealps
publisher HAL CCSD
publishDate 2022
url https://hal.inrae.fr/hal-03790287
https://doi.org/10.1177/03091333221107624
genre permafrost
genre_facet permafrost
op_source ISSN: 0309-1333
Progress in Physical Geography
https://hal.inrae.fr/hal-03790287
Progress in Physical Geography, 2022, ⟨10.1177/03091333221107624⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1177/03091333221107624
hal-03790287
https://hal.inrae.fr/hal-03790287
doi:10.1177/03091333221107624
WOS: 000821104500001
op_doi https://doi.org/10.1177/03091333221107624
container_title Progress in Physical Geography: Earth and Environment
container_volume 47
container_issue 1
container_start_page 50
op_container_end_page 73
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spelling ftunivlimoges:oai:HAL:hal-03790287v1 2024-04-21T08:10:15+00:00 Limited impacts of global warming on rockfall activity at low elevations: Insights from two calcareous cliffs from the French Prealps Mainieri, Robin Eckert, Nicolas Corona, Christophe Lopez-Saez, Jerome Stoffel, Markus Bourrier, Franck Ecosystèmes montagnards (UR EMGR) Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA) Laboratoire des EcoSystèmes et des Sociétés en Montagne (UR LESSEM) Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE) Institut des Géosciences de l’Environnement (IGE) Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP ) Université Grenoble Alpes (UGA) Erosion torrentielle neige et avalanches (UR ETGR (ETNA)) Institute for Environmental Sciences Geneva (ISE) Université de Genève = University of Geneva (UNIGE) Laboratoire de Géographie Physique et Environnementale (GEOLAB) Université Blaise Pascal - Clermont-Ferrand 2 (UBP)-Institut Sciences de l'Homme et de la Société (IR SHS UNILIM) Université de Limoges (UNILIM)-Université de Limoges (UNILIM)-Université Clermont Auvergne 2017-2020 (UCA 2017-2020 )-Centre National de la Recherche Scientifique (CNRS)-Université Clermont Auvergne (UCA) Dendrolab.ch Bern Institute of Geological Sciences Bern Universität Bern / University of Bern (UNIBE)-Universität Bern / University of Bern (UNIBE) ANR-15-IDEX-02 2022 https://hal.inrae.fr/hal-03790287 https://doi.org/10.1177/03091333221107624 en eng HAL CCSD SAGE Publications info:eu-repo/semantics/altIdentifier/doi/10.1177/03091333221107624 hal-03790287 https://hal.inrae.fr/hal-03790287 doi:10.1177/03091333221107624 WOS: 000821104500001 ISSN: 0309-1333 Progress in Physical Geography https://hal.inrae.fr/hal-03790287 Progress in Physical Geography, 2022, ⟨10.1177/03091333221107624⟩ Rockfall tree-ring reconstruction climate change calcareous French Alps [SDE.IE]Environmental Sciences/Environmental Engineering [SDV]Life Sciences [q-bio] info:eu-repo/semantics/article Journal articles 2022 ftunivlimoges https://doi.org/10.1177/03091333221107624 2024-04-10T23:42:38Z International audience In mountainous regions, global warming will likely affect the frequency and magnitude of geomorphic processes. This is also the case for rockfall, one of the most common mass movements on steep slopes. Rainfall, snowmelt, or freeze-thaw cycles are the main drivers of rockfall activity, rockfall hazards are thus generally thought to become more relevant in a context of climate change. At high elevations, unequivocal relationships have been found between increased rockfall activity, permafrost thawing and global warming. By contrast, below the permafrost limit, studies are scarcer. They mostly rely on short or incomplete rockfall records, and have so far failed to identify climatically induced trends in rockfall records. Here, using a dendrogeomorphic approach, we develop two continuous 60-year long chronologies of rockfall activity in the Vercors and Diois massifs (French Alps); both sites are located clearly below the permafrost limit. Uncertainties related to the decreasing number of trees available back in time were quantified based on a detailed mapping of trees covering the slope across time. Significant multiple regression models with reconstructed rockfalls as predictors and local changes in climatic conditions since 1959 extracted from the SAFRAN reanalysis dataset as predictants were fitted to investigate the potential impacts of global warming on rockfall activity at both sites. In the Vercors massif, the strong increase in reconstructed rockfall can be ascribed to the recolonization of the forest stand and the over-representation of young trees; changes that are observed should not therefore be ascribed to climatic fluctuations. In the Diois massif, we identify annual precipitation totals and mean temperatures as statistically significant drivers of rockfall activity but no significant increasing trend was identified in the reconstruction. All in all, despite the stringency of our approach, we cannot therefore confirm that rockfall hazard will increase as a result of global ... Article in Journal/Newspaper permafrost Université de Limoges: HAL Progress in Physical Geography: Earth and Environment 47 1 50 73