Snow and avalanche climates in the French Alps using avalanche problem frequencies

Avalanches result from an interaction of weather and terrain, where past weather and internal snow cover processes play important roles. So far, climatology was mainly based on weather data, as regional snow instability information, such as avalanche activity, is scarce on climatological time scales...

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Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Benjamin Reuter, Pascal Hagenmuller, Nicolas Eckert
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2023
Subjects:
Online Access:https://doi.org/10.1017/jog.2023.23
https://doaj.org/article/d4a16331381546f2a5ff075eb48ad34c
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spelling ftdoajarticles:oai:doaj.org/article:d4a16331381546f2a5ff075eb48ad34c 2023-11-12T04:19:55+01:00 Snow and avalanche climates in the French Alps using avalanche problem frequencies Benjamin Reuter Pascal Hagenmuller Nicolas Eckert 2023-10-01T00:00:00Z https://doi.org/10.1017/jog.2023.23 https://doaj.org/article/d4a16331381546f2a5ff075eb48ad34c EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143023000230/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2023.23 0022-1430 1727-5652 https://doaj.org/article/d4a16331381546f2a5ff075eb48ad34c Journal of Glaciology, Vol 69, Pp 1292-1304 (2023) Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2023 ftdoajarticles https://doi.org/10.1017/jog.2023.23 2023-10-29T00:40:50Z Avalanches result from an interaction of weather and terrain, where past weather and internal snow cover processes play important roles. So far, climatology was mainly based on weather data, as regional snow instability information, such as avalanche activity, is scarce on climatological time scales. We present a new approach to create a snow avalanche climatology from simulations of avalanche problem types based on snow cover simulations of reanalysis data and a cluster analysis. Analyzing the winters between 1958 and 2020 in the French Alps, wet-snow situations dominated natural release. Dry-snow situations with non-persistent and persistent weak layers occurred each on at least one third of the days. Four typical patterns of avalanche problem types were identified. They follow the main orography with more new snow situations in the northern regions and more cases of persistent weak layers in inner-Alpine regions. In the front-ranges and in southern regions wet-snow situations occurred early in winter – typical for coastal snow climates. Agreement with the standard snow climate classification and the geography of the French Alps suggests that mountain regions with similar conditions can now be outlined. This method for snow avalanche climatology will inform avalanche forecasting and facilitate climate change impact studies. Article in Journal/Newspaper Journal of Glaciology Directory of Open Access Journals: DOAJ Articles Journal of Glaciology 69 277 1292 1304
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
spellingShingle Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
Benjamin Reuter
Pascal Hagenmuller
Nicolas Eckert
Snow and avalanche climates in the French Alps using avalanche problem frequencies
topic_facet Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
description Avalanches result from an interaction of weather and terrain, where past weather and internal snow cover processes play important roles. So far, climatology was mainly based on weather data, as regional snow instability information, such as avalanche activity, is scarce on climatological time scales. We present a new approach to create a snow avalanche climatology from simulations of avalanche problem types based on snow cover simulations of reanalysis data and a cluster analysis. Analyzing the winters between 1958 and 2020 in the French Alps, wet-snow situations dominated natural release. Dry-snow situations with non-persistent and persistent weak layers occurred each on at least one third of the days. Four typical patterns of avalanche problem types were identified. They follow the main orography with more new snow situations in the northern regions and more cases of persistent weak layers in inner-Alpine regions. In the front-ranges and in southern regions wet-snow situations occurred early in winter – typical for coastal snow climates. Agreement with the standard snow climate classification and the geography of the French Alps suggests that mountain regions with similar conditions can now be outlined. This method for snow avalanche climatology will inform avalanche forecasting and facilitate climate change impact studies.
format Article in Journal/Newspaper
author Benjamin Reuter
Pascal Hagenmuller
Nicolas Eckert
author_facet Benjamin Reuter
Pascal Hagenmuller
Nicolas Eckert
author_sort Benjamin Reuter
title Snow and avalanche climates in the French Alps using avalanche problem frequencies
title_short Snow and avalanche climates in the French Alps using avalanche problem frequencies
title_full Snow and avalanche climates in the French Alps using avalanche problem frequencies
title_fullStr Snow and avalanche climates in the French Alps using avalanche problem frequencies
title_full_unstemmed Snow and avalanche climates in the French Alps using avalanche problem frequencies
title_sort snow and avalanche climates in the french alps using avalanche problem frequencies
publisher Cambridge University Press
publishDate 2023
url https://doi.org/10.1017/jog.2023.23
https://doaj.org/article/d4a16331381546f2a5ff075eb48ad34c
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology, Vol 69, Pp 1292-1304 (2023)
op_relation https://www.cambridge.org/core/product/identifier/S0022143023000230/type/journal_article
https://doaj.org/toc/0022-1430
https://doaj.org/toc/1727-5652
doi:10.1017/jog.2023.23
0022-1430
1727-5652
https://doaj.org/article/d4a16331381546f2a5ff075eb48ad34c
op_doi https://doi.org/10.1017/jog.2023.23
container_title Journal of Glaciology
container_volume 69
container_issue 277
container_start_page 1292
op_container_end_page 1304
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