Empirical α-β runout modelling of snow avalanches in the Catalan Pyrenees.
A variation in the α−β model which is a regression model that allows a deterministic prediction of the extreme runout to be expected in a given path, was applied for calculating avalanche runout in the Catalan Pyrenees. Present knowledge of major avalanche activity in this region and current mapping...
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International Glaciological Society.
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ftubarcepubl:oai:diposit.ub.edu:2445/179964 2024-02-11T10:05:23+01:00 Empirical α-β runout modelling of snow avalanches in the Catalan Pyrenees. Oller i Figueras, Pere Baeza, Cristina Furdada i Bellavista, Glòria 2021-04 12 p. application/pdf http://hdl.handle.net/2445/179964 eng eng International Glaciological Society. Reproducció del document publicat a: https://doi.org/10.1017/jog.2021.50 Journal of Glaciology, 2021, p. 1-12 Articles publicats en revistes (Dinàmica de la Terra i l'Oceà) https://doi.org/10.1017/jog.2021.50 0022-1430 http://hdl.handle.net/2445/179964 713450 cc-by (c) Oller i Figueras, Pere et al., 2021 https://creativecommons.org/licenses/by/4.0/ info:eu-repo/semantics/openAccess Allaus Pirineus Avalanches Pyrenees info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2021 ftubarcepubl https://doi.org/10.1017/jog.2021.50 2024-01-24T01:15:55Z A variation in the α−β model which is a regression model that allows a deterministic prediction of the extreme runout to be expected in a given path, was applied for calculating avalanche runout in the Catalan Pyrenees. Present knowledge of major avalanche activity in this region and current mapping tools were used. The model was derived using a dataset of 97 'extreme' avalanches that occurred from the end of 19th century to the beginning of 21st century. A multiple linear regression model was obtained using three independent variables: inclination of the avalanche path, horizontal length and area of the starting one, with a good fit of the function (R2 = 0.81). A larger starting zone increases the runout and a larger length of the path reduces the runout. The new updated equation predicts avalanche runout for a return period of ∼100 years. To study which terrain variables explain the extreme values of the avalanche dataset, a comparative analysis of variables that influence a longer or shorter runout was performed. The most extreme avalanches were treated. The size of the avalanche path and the aspect of the starting zone showed certain association between avalanches with longer or shorter runouts. Article in Journal/Newspaper Journal of Glaciology Dipòsit Digital de la Universitat de Barcelona Journal of Glaciology 67 266 1043 1054 |
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Open Polar |
collection |
Dipòsit Digital de la Universitat de Barcelona |
op_collection_id |
ftubarcepubl |
language |
English |
topic |
Allaus Pirineus Avalanches Pyrenees |
spellingShingle |
Allaus Pirineus Avalanches Pyrenees Oller i Figueras, Pere Baeza, Cristina Furdada i Bellavista, Glòria Empirical α-β runout modelling of snow avalanches in the Catalan Pyrenees. |
topic_facet |
Allaus Pirineus Avalanches Pyrenees |
description |
A variation in the α−β model which is a regression model that allows a deterministic prediction of the extreme runout to be expected in a given path, was applied for calculating avalanche runout in the Catalan Pyrenees. Present knowledge of major avalanche activity in this region and current mapping tools were used. The model was derived using a dataset of 97 'extreme' avalanches that occurred from the end of 19th century to the beginning of 21st century. A multiple linear regression model was obtained using three independent variables: inclination of the avalanche path, horizontal length and area of the starting one, with a good fit of the function (R2 = 0.81). A larger starting zone increases the runout and a larger length of the path reduces the runout. The new updated equation predicts avalanche runout for a return period of ∼100 years. To study which terrain variables explain the extreme values of the avalanche dataset, a comparative analysis of variables that influence a longer or shorter runout was performed. The most extreme avalanches were treated. The size of the avalanche path and the aspect of the starting zone showed certain association between avalanches with longer or shorter runouts. |
format |
Article in Journal/Newspaper |
author |
Oller i Figueras, Pere Baeza, Cristina Furdada i Bellavista, Glòria |
author_facet |
Oller i Figueras, Pere Baeza, Cristina Furdada i Bellavista, Glòria |
author_sort |
Oller i Figueras, Pere |
title |
Empirical α-β runout modelling of snow avalanches in the Catalan Pyrenees. |
title_short |
Empirical α-β runout modelling of snow avalanches in the Catalan Pyrenees. |
title_full |
Empirical α-β runout modelling of snow avalanches in the Catalan Pyrenees. |
title_fullStr |
Empirical α-β runout modelling of snow avalanches in the Catalan Pyrenees. |
title_full_unstemmed |
Empirical α-β runout modelling of snow avalanches in the Catalan Pyrenees. |
title_sort |
empirical α-β runout modelling of snow avalanches in the catalan pyrenees. |
publisher |
International Glaciological Society. |
publishDate |
2021 |
url |
http://hdl.handle.net/2445/179964 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_relation |
Reproducció del document publicat a: https://doi.org/10.1017/jog.2021.50 Journal of Glaciology, 2021, p. 1-12 Articles publicats en revistes (Dinàmica de la Terra i l'Oceà) https://doi.org/10.1017/jog.2021.50 0022-1430 http://hdl.handle.net/2445/179964 713450 |
op_rights |
cc-by (c) Oller i Figueras, Pere et al., 2021 https://creativecommons.org/licenses/by/4.0/ info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1017/jog.2021.50 |
container_title |
Journal of Glaciology |
container_volume |
67 |
container_issue |
266 |
container_start_page |
1043 |
op_container_end_page |
1054 |
_version_ |
1790602394942308352 |