dc.contributor.author | Norem, Harald | |
dc.date.accessioned | 2023-08-01T08:43:29Z | |
dc.date.available | 2023-08-01T08:43:29Z | |
dc.date.issued | 1995-10-20 | |
dc.identifier.uri | https://hdl.handle.net/11250/3082062 | |
dc.description.abstract | Full-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.sponsorship | Norges Forskningsråd (NFR) | en_US |
dc.language.iso | eng | en_US |
dc.publisher | Norges Geotekniske Institutt | en_US |
dc.relation.ispartofseries | NGI-rapport;581240-03 | |
dc.rights | Navngivelse 4.0 Internasjonal | * |
dc.rights.uri | http://creativecommons.org/licenses/by/4.0/deed.no | * |
dc.subject | Avalanche-RnD | en_US |
dc.subject | Snøskred-FoU | en_US |
dc.subject | Snow Avalanche | en_US |
dc.subject | snow | en_US |
dc.subject | Dynamic Load | en_US |
dc.subject | Shear Stress | en_US |
dc.subject | Flow | en_US |
dc.subject | Model | en_US |
dc.title | Shear stresses and boundary layers in snow avalanches | en_US |
dc.type | Research report | en_US |
dc.source.pagenumber | 27 | en_US |
dc.relation.project | Avalanche Austria - Switzerland - Norway | en_US |