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dc.contributor.authorGauer, Peter
dc.date.accessioned2019-02-05T08:46:17Z
dc.date.available2019-02-05T08:46:17Z
dc.date.created2019-01-28T10:23:07Z
dc.date.issued2018
dc.identifier.urihttp://hdl.handle.net/11250/2583851
dc.description.abstractAvalanche observations from Norway, Austria and Switzerland, which distinguish between dense (fluidized) flow and powder part, are analyzed to obtain probability information about the reach of the powder part. The analysis suggests that the relative run-out distance of the powder part increases with increasing mean slope angle of the track. The data provide useful hints for avalanche practitioners about the reach and the corresponding probabilities of the powder part of avalanches.
dc.language.isoeng
dc.subjectAvalanche-RnD
dc.subjectSnøskred-FoU
dc.titleEstimates on the reach of the powder part of avalanches
dc.typeLecture
dc.description.versionpublishedVersion
dc.identifier.doihttp://arc.lib.montana.edu/snow-science/item/2654
dc.identifier.cristin1665981
cristin.unitcode7452,3,1,0
cristin.unitnameSnø- og steinskred
cristin.ispublishedtrue
cristin.fulltextoriginal


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