Complementary Notes on My Previous Paper “On a Theory of Turbulence”, and its Application to the Theory of the Daily Range of the Atmospheric Temperature

[摘要] The diffusion in the turbulent flow was discussed in the previous work starting from the analogous equation of the Brownian movement. The application to the diffusion in the atmosphere was tried in this paper and found that the diffusion is not isotropic and the horizontal diffusion coefficinet is much larger than the vertical one. (about one hundred of the latter) The dependency of the vertical diffusion on the lapse rate of the temperature was introduced, and the results agree approximately with the observation which is obtained from the daily range of the atmosphere.

[学科分类] 大气科学