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The Momentum Turbulent Counter-Gradient Transport in Jet-like Flows
作者姓名:V.  N.  Lykossov
作者单位:Institute of
摘    要:Ⅰ. INTRODUCTIONIt is very well known from the observations that some atmospheric motions are accompanied by jets in the boundary layer, for example, breezes and circulations in the mountain valleys (Gutman, 1969); nocturnal increasing of wind (Byzova et al., 1989); cross-equatorial flow during the summer Indian monsoon (Das, 1986) and others. One of the important questions concerning a mathematical modelling of such motions is the problem of the turbulent closure of the equations set which describes the jet dynamics. It is still popular to use for the momentum turbulent flow (u'w') a closure, based within the framework of K-theory on the Boussinesq hypothesis


The Momentum Turbulent Counter-Gradient Transport in Jet-like Flows
V. N. Lykossov.The Momentum Turbulent Counter-Gradient Transport in Jet-like Flows[J].Advances in Atmospheric Sciences,1992,9(2):191-200.
Authors:V N Lykossov
Institution:Institute of Numerical Mathematics, USSR Academy of Sciences, Moscow, USSR
Abstract:
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