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dc.contributor.authorBrabec, Bernhard
dc.contributor.authorStucki, Thomas
dc.contributor.editorHestnes, Erik
dc.date.accessioned2023-08-03T19:50:10Z
dc.date.available2023-08-03T19:50:10Z
dc.date.issued1998
dc.identifier.isbn82-546-0184-4
dc.identifier.issn0078-1193
dc.identifier.urihttps://hdl.handle.net/11250/3082560
dc.description.abstractThe paper describes how avalanche bulletins (regional and national) are being verified by means of questionnaires in Switzerland. At the beginning of winter 1996/97 a set of four questionnaires has been introduced: • Questionnaire A: "Personal judgement of avalanche danger" • Questionnaire B: "Observations of avalanches without personal or material damage" • Questionnaire C: "Observations of avalanches with people caught but without material damage" • Questionnaire D: "Observations of avalanches with personal and/or material damage" About 10000 of these questionnaires have been distributed to the public, 500 have been returned during the winter 1996/97. This means twice as many returns as for previous winters. Questionnaires B,C and D can be used for the verification of the higher hazard degrees. Questionnaire A is the most frequently returned and can be used for all degrees of hazard. Therefore it is the subject of our evaluation. The questionnaires are used on a daily basis for the construction of the bulletin if they were returned in time. Therefore we cannot talk of an independent verification in a strict sense. At the end of the winter a comparison between questionnaires and bulletins has been done. The questionnaires allow to define a degree of hazard for 8 expositions and 4 height zones (lSOO-2000m, 2000-2S00m, 2500- 3000m and >3000m). Therefore we compare a set of 32 segments of every questionnaire to the bulletin. The overall estimation for Switzerland shows that about 64% of the feedback are in agreement with the bulletin, 32% differ by l degree of hazard and 4% by 2. The symmetric distribution of differences indicates that the degree of hazard is neither systematically over- nor underestimated. The distribution varies heavily between regions, height levels and expositions. For the region Davos a detailed verification using additional own field observations has been done and is compared to the verification based on questionnaires.en_US
dc.language.isoengen_US
dc.publisherNorwegian Geotechnical Instituteen_US
dc.relation.ispartofseriesNGI Publication;203
dc.subjectSnow Avalancheen_US
dc.subjectHistoryen_US
dc.subjectAvalanche-RnDen_US
dc.subjectSnøskred-FoUen_US
dc.titleVerification of avalanche bulletins by questionnairesen_US
dc.typeChapteren_US
dc.source.pagenumber79-83en_US


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