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dc.contributor.advisorHestnes, Erik
dc.contributor.authorDomaas, Ulrik
dc.contributor.authorHarbitz, Carl Bonnevie
dc.date.accessioned2023-08-03T19:49:40Z
dc.date.available2023-08-03T19:49:40Z
dc.date.issued1998
dc.identifier.isbn82-546-0184-4
dc.identifier.issn0078-1193
dc.identifier.urihttps://hdl.handle.net/11250/3082555
dc.description.abstractThis article reports on the observed run-up heights of avalanches in terrain formations that act as "natural deflecting dams" with oblique angle of incidence. To compensate for the deficiencies of today's methods, the parameters governing the run-up heights is discussed, and a computational model based on the Voellmy-Perla equation is used for calculation of the avalanche centre-af-mass path along the deflecting dam wall. The maximum calculated centre-af-mass run-up heights of the avalanches are compared with the observed total run-up heights. The relation between the two types of heights is elaborated upon for various categories of slide volumes.en_US
dc.language.isoengen_US
dc.publisherNorwegian Geotechnical Instituteen_US
dc.relation.ispartofseriesNGI Publication;203
dc.subjectSnow Avalancheen_US
dc.subjectDamen_US
dc.subjectRunout Distanceen_US
dc.subjectAvalanche-RnDen_US
dc.subjectSnøskred-FoUen_US
dc.titleOn avalanche run-up heights on deflecting dams: Centre of mass computations compared to observations.en_US
dc.title.alternativeOn avalanche run-up heights on deflecting dams: Centre of mass computations compared to observations.en_US
dc.typeChapteren_US
dc.source.pagenumber94-98en_US


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