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Stationary Model of Wind Distribution with Height in the Atmospheric Boundary Layer

机译：大气边界层高度风分布的平稳模型

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摘要

An approximation method consisting of expansion of the hydrodynamic equation for the boundary layer in terms of small parameters is used to solve the problem of wind distribution with height in the case of curvilinear isobars (a family of second order curves). The reduced curvatures of the isobars are considered as small parameters. The equation of steady motion of an incompressible fluid in the boundary layer of the earth in the case of a constant mixing coefficient is given. Graphs of the plane divergence for the boundary layer of a thickness of 1.5 km for linear and nonlinear cases are presented. (Author)

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Krivosheev, V. L.;
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年度 1969
页码 p.1-17
总页数 17
原文格式 PDF
正文语种 eng
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关键词
Atmosphere ; Wind ; Boundary layer ; Distribution ; Atmosphere models ; Equations of motion ; Approximation(Mathematics) ; Weather forecasting ; Thickness ; Hydrodynamics ; USSR;

机译：大气;风;边界层;分布;大气模型;运动方程;近似（数学）;天气预报;厚度;流体动力学;苏联;

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Stationary Model of Wind Distribution with Height in the Atmospheric Boundary Layer

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