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dc.contributor.authorNorem, Harald
dc.contributor.authorlrgens, Fridtjov
dc.contributor.authorSchieldrop, Bonsak
dc.date.accessioned2023-09-19T17:29:50Z
dc.date.available2023-09-19T17:29:50Z
dc.date.issued1989
dc.identifier.issn1727-5644
dc.identifier.urihttps://hdl.handle.net/11250/3090614
dc.description.abstractThe authors of this paper have previously, in 1987, outlined the development of a set of constitutive equations representing the behaviour of avalanching snow, and the resulting equations for fully developed steady shear flow. The present paper considers the development of non-steady two dimensional shear flow together with the use of a finite-difference programme to calculate snow-avalanche velocities and flow heights in the run-out zone. The numerical results thus obtained are compared with full-scale experimental data. These comparisons indicate that front velocity and run-out distance are simulated well by the model, and thaI the predicted snow deposits are fairly well in agreement with those actually observed.en_US
dc.language.isoengen_US
dc.publisherCambridge University Pressen_US
dc.subjectSnow Avalancheen_US
dc.subjectVelocityen_US
dc.subjectRunout Distanceen_US
dc.subjectAvalanche-RnDen_US
dc.subjectSnøskred-FoUen_US
dc.titleSimulation of snow-avalanche flow in run-out zones.en_US
dc.typeJournal articleen_US
dc.rights.holderInternational Glaciological Societyen_US
dc.source.pagenumber218-225en_US
dc.source.volume13en_US
dc.source.journalAnnals of Glaciologyen_US
dc.identifier.doi10.3189/S026030550000793X


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