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Shear stresses and boundary layers in snow avalanches

dc.contributor.authorNorem, Harald
dc.date.accessioned2023-08-01T08:43:29Z
dc.date.available2023-08-01T08:43:29Z
dc.date.issued1995-10-20
dc.identifier.urihttps://hdl.handle.net/11250/3082062
dc.description.abstractFull-scale experiments on snow avalanches have shown that the major part ofthe avalanches are mixed flow avalanches, and that they consist of at least two parts, a dense flow part and a turbidity part. The report is based on that a fully developed avalanche can be divided in four flow layers.
dc.description.sponsorshipNorges Forskningsråd (NFR)en_US
dc.language.isoengen_US
dc.publisherNorges Geotekniske Institutten_US
dc.relation.ispartofseriesNGI-rapport;581240-03
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.subjectAvalanche-RnDen_US
dc.subjectSnøskred-FoUen_US
dc.subjectSnow Avalancheen_US
dc.subjectsnowen_US
dc.subjectDynamic Loaden_US
dc.subjectShear Stressen_US
dc.subjectFlowen_US
dc.subjectModelen_US
dc.titleShear stresses and boundary layers in snow avalanchesen_US
dc.typeResearch reporten_US
dc.source.pagenumber27en_US
dc.relation.projectAvalanche Austria - Switzerland - Norwayen_US


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Except where otherwise noted, this item's license is described as Navngivelse 4.0 Internasjonal