Scaling relationships for constant-volume snow avalanches

International audience We present simple scaling relationships that allow us to predict the main dynamical characteristics (height, length and velocity) of constant-volume snow avalanches with minimal input data. In particular, we show that both avalanche height and length can be expressed as a func...

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Published in:Annals of Glaciology
Main Authors: Chambon, Guillaume, Naaim, Mohamed
Other Authors: Érosion torrentielle, neige et avalanches (UR ETGR (ETNA)), Centre national du machinisme agricole, du génie rural, des eaux et forêts (CEMAGREF), French National Research Agency (ANR)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2010
Subjects:
Online Access:https://hal.inrae.fr/hal-02592334
https://doi.org/10.3189/172756410791386562
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spelling ftccsdartic:oai:HAL:hal-02592334v1 2023-05-15T13:29:13+02:00 Scaling relationships for constant-volume snow avalanches Lois d'échelle pour des avalanches de neige à volume constant Chambon, Guillaume Naaim, Mohamed Érosion torrentielle, neige et avalanches (UR ETGR (ETNA)) Centre national du machinisme agricole, du génie rural, des eaux et forêts (CEMAGREF) French National Research Agency (ANR) 2010 https://hal.inrae.fr/hal-02592334 https://doi.org/10.3189/172756410791386562 en eng HAL CCSD International Glaciological Society info:eu-repo/semantics/altIdentifier/doi/10.3189/172756410791386562 hal-02592334 https://hal.inrae.fr/hal-02592334 doi:10.3189/172756410791386562 IRSTEA: PUB00027236 WOS: 000281033900019 ISSN: 0260-3055 Annals of Glaciology https://hal.inrae.fr/hal-02592334 Annals of Glaciology, International Glaciological Society, 2010, 51 (54), pp.129-138. ⟨10.3189/172756410791386562⟩ LOI DE VOELLMY SOLUTION AUTOSIMILAIRE MODELE DE SAINT-VENANT LOI D'ECHELLE [SDE]Environmental Sciences info:eu-repo/semantics/article Journal articles 2010 ftccsdartic https://doi.org/10.3189/172756410791386562 2021-08-07T23:06:14Z International audience We present simple scaling relationships that allow us to predict the main dynamical characteristics (height, length and velocity) of constant-volume snow avalanches with minimal input data. In particular, we show that both avalanche height and length can be expressed as a function of the avalanche volume and the distance travelled by the front, independent of the specific rheological parameters of the snow. These scaling relationships are derived from a large-time asymptotic solution to the avalanche dynamic equations, corresponding to a balance between gravity and Voellmy friction (the kinematic wave approximation). Numerical simulations of the complete hydraulic shallow-flow equations confirm that this asymptotic solution, and the predicted scaling relationships, capture the main avalanche characteristics, even for relatively small travel distances. Though derived under restrictive assumptions, we argue that the scaling relationships described in this paper may constitute useful tools for avalanche engineering and design of protective structures. Article in Journal/Newspaper Annals of Glaciology Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Annals of Glaciology 51 54 129 138
institution Open Polar
collection Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe)
op_collection_id ftccsdartic
language English
topic LOI DE VOELLMY
SOLUTION AUTOSIMILAIRE
MODELE DE SAINT-VENANT
LOI D'ECHELLE
[SDE]Environmental Sciences
spellingShingle LOI DE VOELLMY
SOLUTION AUTOSIMILAIRE
MODELE DE SAINT-VENANT
LOI D'ECHELLE
[SDE]Environmental Sciences
Chambon, Guillaume
Naaim, Mohamed
Scaling relationships for constant-volume snow avalanches
topic_facet LOI DE VOELLMY
SOLUTION AUTOSIMILAIRE
MODELE DE SAINT-VENANT
LOI D'ECHELLE
[SDE]Environmental Sciences
description International audience We present simple scaling relationships that allow us to predict the main dynamical characteristics (height, length and velocity) of constant-volume snow avalanches with minimal input data. In particular, we show that both avalanche height and length can be expressed as a function of the avalanche volume and the distance travelled by the front, independent of the specific rheological parameters of the snow. These scaling relationships are derived from a large-time asymptotic solution to the avalanche dynamic equations, corresponding to a balance between gravity and Voellmy friction (the kinematic wave approximation). Numerical simulations of the complete hydraulic shallow-flow equations confirm that this asymptotic solution, and the predicted scaling relationships, capture the main avalanche characteristics, even for relatively small travel distances. Though derived under restrictive assumptions, we argue that the scaling relationships described in this paper may constitute useful tools for avalanche engineering and design of protective structures.
author2 Érosion torrentielle, neige et avalanches (UR ETGR (ETNA))
Centre national du machinisme agricole, du génie rural, des eaux et forêts (CEMAGREF)
French National Research Agency (ANR)
format Article in Journal/Newspaper
author Chambon, Guillaume
Naaim, Mohamed
author_facet Chambon, Guillaume
Naaim, Mohamed
author_sort Chambon, Guillaume
title Scaling relationships for constant-volume snow avalanches
title_short Scaling relationships for constant-volume snow avalanches
title_full Scaling relationships for constant-volume snow avalanches
title_fullStr Scaling relationships for constant-volume snow avalanches
title_full_unstemmed Scaling relationships for constant-volume snow avalanches
title_sort scaling relationships for constant-volume snow avalanches
publisher HAL CCSD
publishDate 2010
url https://hal.inrae.fr/hal-02592334
https://doi.org/10.3189/172756410791386562
genre Annals of Glaciology
genre_facet Annals of Glaciology
op_source ISSN: 0260-3055
Annals of Glaciology
https://hal.inrae.fr/hal-02592334
Annals of Glaciology, International Glaciological Society, 2010, 51 (54), pp.129-138. ⟨10.3189/172756410791386562⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.3189/172756410791386562
hal-02592334
https://hal.inrae.fr/hal-02592334
doi:10.3189/172756410791386562
IRSTEA: PUB00027236
WOS: 000281033900019
op_doi https://doi.org/10.3189/172756410791386562
container_title Annals of Glaciology
container_volume 51
container_issue 54
container_start_page 129
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