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dc.contributor.authorNishimura, K.
dc.contributor.authorPérez-Guillén, Cristina
dc.contributor.authorIto, Yoichi
dc.contributor.authorYamaguchi, Satoru
dc.contributor.authorSaito, Yoshihiko
dc.contributor.authorIssler, Dieter
dc.contributor.authorFischer, Jan-Thomas
dc.date.accessioned2019-02-05T08:45:32Z
dc.date.available2019-02-05T08:45:32Z
dc.date.created2019-01-29T15:24:23Z
dc.date.issued2018
dc.identifier.urihttp://hdl.handle.net/11250/2583848
dc.description.abstractSystematic full-scale but small avalanche experiments have been started since 2016 in Niseko, a ski resort in Hokkaido, Japan. Although the vertical drop in the test sites are 100 to 200 m, they have advantages that we are able to access relatively easy and can expect both dry avalanches in February and wet ones in March. On top of that, it has a potential that we can look at the phenomena closer and investigate the detailed structures and mechanism of avalanches. Although the artificial releases and measurements were not always successful so far, data for three wet snow avalanches were obtained and they revealed that the combination of different data is effective measures to characterize their structures.
dc.language.isoeng
dc.subjectAvalanche-RnD
dc.subjectSnøskred-FoU
dc.titleStudies on the snow avalanche dynamics by the full-scale experiments
dc.typeLecture
dc.description.versionpublishedVersion
dc.identifier.doihttp://arc.lib.montana.edu/snow-science/objects/ISSW2018_P01.8.pdf
dc.identifier.cristin1667792
cristin.unitcode7452,3,1,0
cristin.unitnameSnø- og steinskred
cristin.ispublishedtrue
cristin.fulltextoriginal


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