Snow Entrainment Coefficient Estimated by Field Observations and Wind Tunnel Experiments

dc.contributor.author	Takuro Kikuchi
dc.contributor.author	Yusuke Fukushima
dc.contributor.author	Kouichi Nishimura
dc.date.accessioned	2017-05-08T21:14:09Z
dc.date.available	2017-05-08T21:14:09Z
dc.date.copyright	December 2005
dc.date.issued	2005
dc.identifier.other	%28asce%290887-381x%282005%2919%3A4%28117%29.pdf
dc.identifier.uri	http://yetl.yabesh.ir/yetl/handle/yetl/43772
dc.description.abstract	The 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
dc.publisher	American Society of Civil Engineers
dc.title	Snow Entrainment Coefficient Estimated by Field Observations and Wind Tunnel Experiments
dc.type	Journal Paper
dc.journal.volume	19
dc.journal.issue	4
dc.journal.title	Journal of Cold Regions Engineering
dc.identifier.doi	10.1061/(ASCE)0887-381X(2005)19:4(117)
dc.tree	Journal of Cold Regions Engineering:;2005:;Volume ( 019 ):;issue: 004
dc.contenttype	Fulltext