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Associations between shear strength of a buried surface hoar layer and stratigraphic, topographic and vegetation characteristics on a uniform slope. Extended abstract

dc.contributor.authorLutz, Eric
dc.contributor.authorBirkeland, Karl W.
dc.contributor.authorSchneebeli, Martin
dc.contributor.authorHansen, Kathy J.
dc.contributor.authorKronholm, Kalle
dc.date.accessioned2023-09-18T06:01:58Z
dc.date.available2023-09-18T06:01:58Z
dc.date.issued2006
dc.identifier.urihttps://hdl.handle.net/11250/3089945
dc.description.abstractIn this study we quantify 1) changes in spatial and aspatial characteristics of the shear strength of a buried surface hoar layer, and 2) identify characteristics in terrain, vegetation and snow stratigraphy that can help clarify some of the variation in shear strength. The study site is a relatively uniform 31 m by 31 m slope in southwest Montana. A local coordinate system linked terrain, vegetation and snow information.en_US
dc.language.isoengen_US
dc.publisherMontana State University Libraryen_US
dc.relation.ispartofseriesThe International Snow Science Workshop (ISSW) Proceedings;
dc.subjectShear Strengthen_US
dc.subjectSnow Avalancheen_US
dc.subjectAvalanche-RnDen_US
dc.subjectSnøskred-FoUen_US
dc.titleAssociations between shear strength of a buried surface hoar layer and stratigraphic, topographic and vegetation characteristics on a uniform slope. Extended abstracten_US
dc.typeChapteren_US
dc.source.pagenumber27-28en_US


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