水平方向の擴散係數に就いて
1938 年 16 巻 7 号 p. 290-291
詳細
1938 年 16 巻 7 号 p. 290-291
It is proved that the diffusion in the atmosphere is not isotropic and the horizontal diffusion coefficient is much larger than the vertical. In this paper, the horizontal eddy diffusion coefficient was calculated from hourly observation of wind velocity and found that it is about 109.
