Laboratory Simulation of Turbulent Flow in the Lower Part of the Planetary Boundary Layer

概要

論文の詳細を見る
The vertical distribution of horizontal mean wind velocity is approximately described by the power law in the lower atmosphere. In the present paper, a method of intentionally constructing a grid by satisfing an empirical formula between an exponent n of wind profile and grid parameters is proposed and it is also shown that the model wind produced by this method is similar fairly well to the natural wind observed at Minnesota on vertical distributions of horizontal mean wind velocities and turbulent intensities, while vertical distributions of their vertical fluxes of momentum are not similar to each other. However, it is shown that possibility of simulating the last ones of the above-mentioned characteristics by suitable combination of grid parameters is expected.
お茶の水女子大学の論文