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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Published in:Journal of Glaciology
Main Authors: Oller i Figueras, Pere, Baeza, Cristina, Furdada i Bellavista, Glòria
Format: Article in Journal/Newspaper
Language:English
Published: International Glaciological Society. 2021
Subjects:
Online Access:http://hdl.handle.net/2445/179964
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spelling 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
institution 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
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