Abstract
Empirical relation between the turbulent velocity υ and the scale of phenomenon L in the atmosphere is obtained as υ-L1/6 instead of -L1/3 for the wide range including the inertial subrange, which was expected as well as in the ocean. Then Okubo's experimental diffusion relation, K-L1.19 for the wide range, instead of L4/3, is explained by the above relation and the new enercv spectrum and auto-correlation function are proposed.
