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dc.contributor.authorKristensen, Krister
dc.contributor.authorHarbitz, Carl Bonnevie
dc.contributor.authorHarbitz, Alf
dc.coverage.spatialWestern Norwayen_US
dc.date.accessioned2023-08-14T10:46:02Z
dc.date.available2023-08-14T10:46:02Z
dc.date.issued2000
dc.identifier.urihttps://hdl.handle.net/11250/3083773
dc.description.abstractIn avalanche hazard zoning, it is common practice to investigate the previous avalanche history for the area considered. Historical observations of avalanches serve as an aid in the classification of the terrain, and may also serve as verification of estimates of avalanche runout. Conditions influencing the avalanche occurrences may change significantly over time and it is important to take these changes into account when using historical avalanche observations in hazard ioning today. A number of the most extensive avalanches recorded in Norway, are found during the eigthteenth and nineteenth century. The catastrophes may be linked to weather as well as to socio-econornic conditions, in particular deforestation of mountain slopes. The implications of using or disregarding historical avalanche observation are shown in an example of statistical estimation of avalanche runout.en_US
dc.language.isoengen_US
dc.publisherMontana State University Libraryen_US
dc.relation.ispartofseriesThe International Snow Science Workshop (ISSW) Proceedings;
dc.subjectSnøskred-FoUen_US
dc.subjectAvalanche-RnDen_US
dc.subjectStatistical Analysisen_US
dc.subjectRunout Distanceen_US
dc.subjectProbabilityen_US
dc.subjectHazarden_US
dc.subjectSnow Avalancheen_US
dc.subjectWestern Norwayen_US
dc.subjectExtreme Value Statisticsen_US
dc.titleSignificance of historical records for avalanche hazard zoning in Norwayen_US
dc.typeChapteren_US
dc.source.pagenumber475-480 (6s)en_US


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