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 |
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Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Cambridge University Press
1998
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Subjects: | |
Online Access: | https://hdl.handle.net/11250/3090613 https://doi.org/ https://doi.org/10.3189/1998AoG26-1-265-271 |
_version_ | 1821509610908942336 |
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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 |
collection | Norwegian Geotechnical Institute (NGI) Digital Archive |
container_start_page | 265 |
container_title | Annals of Glaciology |
container_volume | 26 |
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 |
genre | Annals of Glaciology |
genre_facet | Annals of Glaciology |
id | ftngi:oai:ngi.brage.unit.no:11250/3090613 |
institution | Open Polar |
language | English |
op_collection_id | ftngi |
op_container_end_page | 271 |
op_doi | https://doi.org/10.3189/1998AoG26-1-265-271 |
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_source | 265-271 26 Annals of Glaciology |
publishDate | 1998 |
publisher | Cambridge University Press |
record_format | openpolar |
spelling | ftngi:oai:ngi.brage.unit.no:11250/3090613 2025-01-16T18:59:46+00:00 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 |
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 |
title | 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_short | Simulations of dense snow avalanches on deflecting dams |
title_sort | simulations of dense snow avalanches on deflecting dams |
topic | Dam Case Record Mathematical Model Numerical Method Simulation Avalanche-RnD Snøskred-FoU |
topic_facet | Dam Case Record Mathematical Model Numerical Method Simulation Avalanche-RnD Snøskred-FoU |
url | https://hdl.handle.net/11250/3090613 https://doi.org/ https://doi.org/10.3189/1998AoG26-1-265-271 |