Simulations of dense snow avalanches on deflecting dams

Two models simulating snow avalanches impacting retaining dams at oblique angles of incidence are presented. First, a lumped-mass model applying the Voellmy-Perla equation is used to calculate the path of the centre-of-mass along the side of a retaining dam. Secondly, a one-dimensional continuum mod...

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Published in:Annals of Glaciology
Main Authors: Irgens, Fridtjov, Schieldrop, Bonsak, Harbitz, Carl Bonnevie, Domaas, Ulrik, Opsahl, Runar
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 1998
Subjects:
Dam
Online Access:https://hdl.handle.net/11250/3090613
https://doi.org/
https://doi.org/10.3189/1998AoG26-1-265-271
id ftngi:oai:ngi.brage.unit.no:11250/3090613
record_format openpolar
spelling ftngi:oai:ngi.brage.unit.no:11250/3090613 2023-10-25T01:29:01+02:00 Simulations of dense snow avalanches on deflecting dams Irgens, Fridtjov Schieldrop, Bonsak Harbitz, Carl Bonnevie Domaas, Ulrik Opsahl, Runar 1998 application/pdf https://hdl.handle.net/11250/3090613 https://doi.org/ https://doi.org/10.3189/1998AoG26-1-265-271 eng eng Cambridge University Press urn:issn:1727-5644 https://hdl.handle.net/11250/3090613 https://doi.org/ https://doi.org/10.3189/1998AoG26-1-265-271 International Glaciological Society 265-271 26 Annals of Glaciology Dam Case Record Mathematical Model Numerical Method Simulation Avalanche-RnD Snøskred-FoU Journal article 1998 ftngi https://doi.org/10.3189/1998AoG26-1-265-271 2023-09-27T22:48:32Z Two models simulating snow avalanches impacting retaining dams at oblique angles of incidence are presented. First, a lumped-mass model applying the Voellmy-Perla equation is used to calculate the path of the centre-of-mass along the side of a retaining dam. Secondly, a one-dimensional continuum model, applying depth-integrated equations of balance of mass and linear momentum, is expanded to take into account that real avalanche flows are three-dimensional. The centre-line of the avalanche path is determined by the flowing material as it progresses down the channelized avalanche path. The nonlinear constitutive equations comprise viscosity, visco-elasticity and plasticity. Both models are calibrated by simulations of a registered avalanche following a strongly curved channel. The path and the run-up height of the avalanche on the natural deflecting dam with oblique angle of incidence as calculated by the two models, are compared with the observations made. Article in Journal/Newspaper Annals of Glaciology Norwegian Geotechnical Institute (NGI) Digital Archive Annals of Glaciology 26 265 271
institution Open Polar
collection Norwegian Geotechnical Institute (NGI) Digital Archive
op_collection_id ftngi
language English
topic Dam
Case Record
Mathematical Model
Numerical Method
Simulation
Avalanche-RnD
Snøskred-FoU
spellingShingle Dam
Case Record
Mathematical Model
Numerical Method
Simulation
Avalanche-RnD
Snøskred-FoU
Irgens, Fridtjov
Schieldrop, Bonsak
Harbitz, Carl Bonnevie
Domaas, Ulrik
Opsahl, Runar
Simulations of dense snow avalanches on deflecting dams
topic_facet Dam
Case Record
Mathematical Model
Numerical Method
Simulation
Avalanche-RnD
Snøskred-FoU
description Two models simulating snow avalanches impacting retaining dams at oblique angles of incidence are presented. First, a lumped-mass model applying the Voellmy-Perla equation is used to calculate the path of the centre-of-mass along the side of a retaining dam. Secondly, a one-dimensional continuum model, applying depth-integrated equations of balance of mass and linear momentum, is expanded to take into account that real avalanche flows are three-dimensional. The centre-line of the avalanche path is determined by the flowing material as it progresses down the channelized avalanche path. The nonlinear constitutive equations comprise viscosity, visco-elasticity and plasticity. Both models are calibrated by simulations of a registered avalanche following a strongly curved channel. The path and the run-up height of the avalanche on the natural deflecting dam with oblique angle of incidence as calculated by the two models, are compared with the observations made.
format Article in Journal/Newspaper
author Irgens, Fridtjov
Schieldrop, Bonsak
Harbitz, Carl Bonnevie
Domaas, Ulrik
Opsahl, Runar
author_facet Irgens, Fridtjov
Schieldrop, Bonsak
Harbitz, Carl Bonnevie
Domaas, Ulrik
Opsahl, Runar
author_sort Irgens, Fridtjov
title Simulations of dense snow avalanches on deflecting dams
title_short Simulations of dense snow avalanches on deflecting dams
title_full Simulations of dense snow avalanches on deflecting dams
title_fullStr Simulations of dense snow avalanches on deflecting dams
title_full_unstemmed Simulations of dense snow avalanches on deflecting dams
title_sort simulations of dense snow avalanches on deflecting dams
publisher Cambridge University Press
publishDate 1998
url https://hdl.handle.net/11250/3090613
https://doi.org/
https://doi.org/10.3189/1998AoG26-1-265-271
genre Annals of Glaciology
genre_facet Annals of Glaciology
op_source 265-271
26
Annals of Glaciology
op_relation urn:issn:1727-5644
https://hdl.handle.net/11250/3090613
https://doi.org/
https://doi.org/10.3189/1998AoG26-1-265-271
op_rights International Glaciological Society
op_doi https://doi.org/10.3189/1998AoG26-1-265-271
container_title Annals of Glaciology
container_volume 26
container_start_page 265
op_container_end_page 271
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