Empirical α – β runout modelling of snow avalanches in the Catalan Pyrenees

Abstract 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 curr...

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Published in:Journal of Glaciology
Main Authors: Oller, Pere, Baeza, Cristina, Furdada, Glòria
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2021
Subjects:
Online Access:http://dx.doi.org/10.1017/jog.2021.50
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143021000502
id crcambridgeupr:10.1017/jog.2021.50
record_format openpolar
spelling crcambridgeupr:10.1017/jog.2021.50 2024-03-03T08:46:07+00:00 Empirical α – β runout modelling of snow avalanches in the Catalan Pyrenees Oller, Pere Baeza, Cristina Furdada, Glòria 2021 http://dx.doi.org/10.1017/jog.2021.50 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143021000502 en eng Cambridge University Press (CUP) http://creativecommons.org/licenses/by-nc-sa/4.0/ Journal of Glaciology volume 67, issue 266, page 1043-1054 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 2021 crcambridgeupr https://doi.org/10.1017/jog.2021.50 2024-02-08T08:43:13Z Abstract 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 zone, with a good fit of the function ( R 2 = 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 Cambridge University Press Journal of Glaciology 1 12
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Oller, Pere
Baeza, Cristina
Furdada, Glòria
Empirical α – β runout modelling of snow avalanches in the Catalan Pyrenees
topic_facet Earth-Surface Processes
description Abstract 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 zone, with a good fit of the function ( R 2 = 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, Pere
Baeza, Cristina
Furdada, Glòria
author_facet Oller, Pere
Baeza, Cristina
Furdada, Glòria
author_sort Oller, 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 Cambridge University Press (CUP)
publishDate 2021
url http://dx.doi.org/10.1017/jog.2021.50
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143021000502
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 67, issue 266, page 1043-1054
ISSN 0022-1430 1727-5652
op_rights http://creativecommons.org/licenses/by-nc-sa/4.0/
op_doi https://doi.org/10.1017/jog.2021.50
container_title Journal of Glaciology
container_start_page 1
op_container_end_page 12
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