Estimation of the kolmogorov constant C0 from classical statistical diffusion theory

The classical statistical diffusion theory and the observed spectral properties are used to estimate the Kolmogorov constant C0 under different stability conditions and for the three velocity components. Such C0 values are related to the shape of the Eulerian velocity spectra and to the ratio between the Lagrangian and Eulerian statistics. The results of this new method of deriving C0 values are shown to be in good agreement with previously determined C0 values in the Planetary Boundary Layer.