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dc.contributor.authorFaug, Thierry
dc.contributor.authorTurnbull, Barbara
dc.contributor.authorGauer, Peter
dc.date.accessioned2023-09-29T09:57:50Z
dc.date.available2023-09-29T09:57:50Z
dc.date.issued2018-03-04
dc.identifier.issn2169-9011
dc.identifier.urihttps://hdl.handle.net/11250/3093027
dc.description.abstractKöhler et al. (2018, https://doi.org/10.1002/2017JF004375) deploy a high spatial and temporal resolution GEODAR radar system to reveal the inside of snow avalanches over the entire slope. They detect a rich variety of longitudinal and slope normal flow structures across a data set of 77 avalanches recorded over 6 years. Distinctive features in the radar signatures permit the definition of seven flow regimes and three distinct stopping signatures, illustrating behaviors much richer than the conventional dichotomy between dense flow avalanches and powder snow avalanches. This presents modelers with the challenge of exploring the physics of these regimes, the transitions between them and their relationship with the surrounding conditions.en_US
dc.language.isoengen_US
dc.publisherAmerican Geophysical Unionen_US
dc.subjectAvalanche-RnDen_US
dc.subjectSnøskred-FoUen_US
dc.titleLooking Beyond the Powder/Dense FlowAvalanche Dichotomyen_US
dc.typeJournal articleen_US
dc.rights.holderAmerican Geophysical Unionen_US
dc.source.pagenumber1181-1496en_US
dc.source.volume123en_US
dc.source.journalJournal of Geophysical Research: Earth Surfaceen_US
dc.source.issue6en_US


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