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contributor authorTakuro Kikuchi
contributor authorYusuke Fukushima
contributor authorKouichi Nishimura
date accessioned2017-05-08T21:14:09Z
date available2017-05-08T21:14:09Z
date copyrightDecember 2005
date issued2005
identifier other%28asce%290887-381x%282005%2919%3A4%28117%29.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/43772
description abstractThe boundary condition for concentration of snow particles at the bed is necessary to calculate snowdrifts by a numerical analysis model. The flux type or the gradient type boundary conditions are reasonable. An idea of an entrainment coefficient of snow particle at the snow surface is useful. The values of the coefficient are considered to be a function of the density and viscosity of the working fluid and the properties of snow particles. In this paper, the values of the coefficient are estimated based on the
publisherAmerican Society of Civil Engineers
titleSnow Entrainment Coefficient Estimated by Field Observations and Wind Tunnel Experiments
typeJournal Paper
journal volume19
journal issue4
journal titleJournal of Cold Regions Engineering
identifier doi10.1061/(ASCE)0887-381X(2005)19:4(117)
treeJournal of Cold Regions Engineering:;2005:;Volume ( 019 ):;issue: 004
contenttypeFulltext


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