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...
Published in: | Annals of Glaciology |
---|---|
Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Cambridge University Press
1998
|
Subjects: | |
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 |
_version_ |
1780730841297584128 |