Saharan dust events in the European Alps: role in snowmelt and geochemical characterization
International audience Abstract. The input of mineral dust from arid regions impacts snow optical properties. The induced albedo reduction generally alters the melting dynamics of the snowpack, resulting in earlier snowmelt. In this paper, we evaluate the impact of dust depositions on the melting dy...
Published in: | The Cryosphere |
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Main Authors: | , , , , , , , , , , , , , , , , , |
Other Authors: | , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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HAL CCSD
2019
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Online Access: | https://hal-meteofrance.archives-ouvertes.fr/meteo-03657896 https://hal-meteofrance.archives-ouvertes.fr/meteo-03657896/document https://hal-meteofrance.archives-ouvertes.fr/meteo-03657896/file/tc-13-1147-2019.pdf https://doi.org/10.5194/tc-13-1147-2019 |
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ftinsu:oai:HAL:meteo-03657896v1 |
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Open Polar |
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Institut national des sciences de l'Univers: HAL-INSU |
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ftinsu |
language |
English |
topic |
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences |
spellingShingle |
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences Di Mauro, Biagio Garzonio, Roberto Rossini, Micol Filippa, Gianluca Pogliotti, Paolo Galvagno, Marta Morra Di Cella, Umberto Migliavacca, Mirco Baccolo, Giovanni Clemenza, Massimiliano Delmonte, Barbara Maggi, Valter Dumont, Marie Tuzet, François Lafaysse, Matthieu Morin, Samuel Cremonese, Edoardo Colombo, Roberto Saharan dust events in the European Alps: role in snowmelt and geochemical characterization |
topic_facet |
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences |
description |
International audience Abstract. The input of mineral dust from arid regions impacts snow optical properties. The induced albedo reduction generally alters the melting dynamics of the snowpack, resulting in earlier snowmelt. In this paper, we evaluate the impact of dust depositions on the melting dynamics of snowpack at a high-elevation site (2160 m) in the European Alps (Torgnon, Aosta Valley, Italy) during three hydrological years (2013–2016). These years were characterized by several Saharan dust events that deposited significant amounts of mineral dust in the European Alps. We quantify the shortening of the snow season due to dust deposition by comparing observed snow depths and those simulated with the Crocus model accounting, or not, for the impact of impurities. The model was run and tested using meteorological data from an automated weather station. We propose the use of repeated digital images for tracking dust deposition and resurfacing in the snowpack. The good agreement between model prediction and digital images allowed us to propose the use of an RGB index (i.e. snow darkening index – SDI) for monitoring dust on snow using images from a digital camera. We also present a geochemical characterization of dust reaching the Alpine chain during spring in 2014. Elements found in dust were classified as a function of their origin and compared with Saharan sources. A strong enrichment in Fe was observed in snow containing Saharan dust. In our case study, the comparison between modelling results and observations showed that impurities deposited in snow anticipated the disappearance of snow up to 38 d a out of a total 7 months of typical snow duration. This happened for the season 2015–2016 that was characterized by a strong dust deposition event. During the other seasons considered here (2013–2014 and 2014–2015), the snow melt-out date was 18 and 11 d earlier, respectively. We conclude that the effect of the Saharan dust is expected to reduce snow cover duration through the snow-albedo feedback. This ... |
author2 |
Centre d'Etudes de la Neige (CEN) 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)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP) 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)-Observatoire des Sciences de l'Univers de Grenoble (OSUG ) Institut national des sciences de l'Univers (INSU - CNRS)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Université Grenoble Alpes (UGA)-Météo-France -Institut national des sciences de l'Univers (INSU - CNRS)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Université Grenoble Alpes (UGA) |
format |
Article in Journal/Newspaper |
author |
Di Mauro, Biagio Garzonio, Roberto Rossini, Micol Filippa, Gianluca Pogliotti, Paolo Galvagno, Marta Morra Di Cella, Umberto Migliavacca, Mirco Baccolo, Giovanni Clemenza, Massimiliano Delmonte, Barbara Maggi, Valter Dumont, Marie Tuzet, François Lafaysse, Matthieu Morin, Samuel Cremonese, Edoardo Colombo, Roberto |
author_facet |
Di Mauro, Biagio Garzonio, Roberto Rossini, Micol Filippa, Gianluca Pogliotti, Paolo Galvagno, Marta Morra Di Cella, Umberto Migliavacca, Mirco Baccolo, Giovanni Clemenza, Massimiliano Delmonte, Barbara Maggi, Valter Dumont, Marie Tuzet, François Lafaysse, Matthieu Morin, Samuel Cremonese, Edoardo Colombo, Roberto |
author_sort |
Di Mauro, Biagio |
title |
Saharan dust events in the European Alps: role in snowmelt and geochemical characterization |
title_short |
Saharan dust events in the European Alps: role in snowmelt and geochemical characterization |
title_full |
Saharan dust events in the European Alps: role in snowmelt and geochemical characterization |
title_fullStr |
Saharan dust events in the European Alps: role in snowmelt and geochemical characterization |
title_full_unstemmed |
Saharan dust events in the European Alps: role in snowmelt and geochemical characterization |
title_sort |
saharan dust events in the european alps: role in snowmelt and geochemical characterization |
publisher |
HAL CCSD |
publishDate |
2019 |
url |
https://hal-meteofrance.archives-ouvertes.fr/meteo-03657896 https://hal-meteofrance.archives-ouvertes.fr/meteo-03657896/document https://hal-meteofrance.archives-ouvertes.fr/meteo-03657896/file/tc-13-1147-2019.pdf https://doi.org/10.5194/tc-13-1147-2019 |
genre |
The Cryosphere |
genre_facet |
The Cryosphere |
op_source |
ISSN: 1994-0424 EISSN: 1994-0416 The Cryosphere https://hal-meteofrance.archives-ouvertes.fr/meteo-03657896 The Cryosphere, 2019, 13 (4), pp.1147-1165. ⟨10.5194/tc-13-1147-2019⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.5194/tc-13-1147-2019 meteo-03657896 https://hal-meteofrance.archives-ouvertes.fr/meteo-03657896 https://hal-meteofrance.archives-ouvertes.fr/meteo-03657896/document https://hal-meteofrance.archives-ouvertes.fr/meteo-03657896/file/tc-13-1147-2019.pdf doi:10.5194/tc-13-1147-2019 |
op_rights |
http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.5194/tc-13-1147-2019 |
container_title |
The Cryosphere |
container_volume |
13 |
container_issue |
4 |
container_start_page |
1147 |
op_container_end_page |
1165 |
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1769009668099670016 |
spelling |
ftinsu:oai:HAL:meteo-03657896v1 2023-06-18T03:43:19+02:00 Saharan dust events in the European Alps: role in snowmelt and geochemical characterization Di Mauro, Biagio Garzonio, Roberto Rossini, Micol Filippa, Gianluca Pogliotti, Paolo Galvagno, Marta Morra Di Cella, Umberto Migliavacca, Mirco Baccolo, Giovanni Clemenza, Massimiliano Delmonte, Barbara Maggi, Valter Dumont, Marie Tuzet, François Lafaysse, Matthieu Morin, Samuel Cremonese, Edoardo Colombo, Roberto Centre d'Etudes de la Neige (CEN) 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)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP) 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)-Observatoire des Sciences de l'Univers de Grenoble (OSUG ) Institut national des sciences de l'Univers (INSU - CNRS)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Université Grenoble Alpes (UGA)-Météo-France -Institut national des sciences de l'Univers (INSU - CNRS)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Université Grenoble Alpes (UGA) 2019 https://hal-meteofrance.archives-ouvertes.fr/meteo-03657896 https://hal-meteofrance.archives-ouvertes.fr/meteo-03657896/document https://hal-meteofrance.archives-ouvertes.fr/meteo-03657896/file/tc-13-1147-2019.pdf https://doi.org/10.5194/tc-13-1147-2019 en eng HAL CCSD Copernicus info:eu-repo/semantics/altIdentifier/doi/10.5194/tc-13-1147-2019 meteo-03657896 https://hal-meteofrance.archives-ouvertes.fr/meteo-03657896 https://hal-meteofrance.archives-ouvertes.fr/meteo-03657896/document https://hal-meteofrance.archives-ouvertes.fr/meteo-03657896/file/tc-13-1147-2019.pdf doi:10.5194/tc-13-1147-2019 http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess ISSN: 1994-0424 EISSN: 1994-0416 The Cryosphere https://hal-meteofrance.archives-ouvertes.fr/meteo-03657896 The Cryosphere, 2019, 13 (4), pp.1147-1165. ⟨10.5194/tc-13-1147-2019⟩ [SDU.STU]Sciences of the Universe [physics]/Earth Sciences info:eu-repo/semantics/article Journal articles 2019 ftinsu https://doi.org/10.5194/tc-13-1147-2019 2023-06-05T20:38:23Z International audience Abstract. The input of mineral dust from arid regions impacts snow optical properties. The induced albedo reduction generally alters the melting dynamics of the snowpack, resulting in earlier snowmelt. In this paper, we evaluate the impact of dust depositions on the melting dynamics of snowpack at a high-elevation site (2160 m) in the European Alps (Torgnon, Aosta Valley, Italy) during three hydrological years (2013–2016). These years were characterized by several Saharan dust events that deposited significant amounts of mineral dust in the European Alps. We quantify the shortening of the snow season due to dust deposition by comparing observed snow depths and those simulated with the Crocus model accounting, or not, for the impact of impurities. The model was run and tested using meteorological data from an automated weather station. We propose the use of repeated digital images for tracking dust deposition and resurfacing in the snowpack. The good agreement between model prediction and digital images allowed us to propose the use of an RGB index (i.e. snow darkening index – SDI) for monitoring dust on snow using images from a digital camera. We also present a geochemical characterization of dust reaching the Alpine chain during spring in 2014. Elements found in dust were classified as a function of their origin and compared with Saharan sources. A strong enrichment in Fe was observed in snow containing Saharan dust. In our case study, the comparison between modelling results and observations showed that impurities deposited in snow anticipated the disappearance of snow up to 38 d a out of a total 7 months of typical snow duration. This happened for the season 2015–2016 that was characterized by a strong dust deposition event. During the other seasons considered here (2013–2014 and 2014–2015), the snow melt-out date was 18 and 11 d earlier, respectively. We conclude that the effect of the Saharan dust is expected to reduce snow cover duration through the snow-albedo feedback. This ... Article in Journal/Newspaper The Cryosphere Institut national des sciences de l'Univers: HAL-INSU The Cryosphere 13 4 1147 1165 |