Diffusion and Scattering in Multifractal Clouds

Turbulent cascade processes generically give rise to asymptotic in between these functions and hence obtain extremely variable multifractals, and there is now the single scattering statistics. In some special cases, it is abundant empirical evidence that both cloud liquid water possible to renormalize the multifractal so as to obtain an density and cloud radiance fields are multifractal over equivalent homogeneous medium. We then estimate wide ranges of scale. Since general circulation models and anomalous diffusion exponents. NWPs assume that clouds are on the contrary horizontally homogeneous, it is therefore important to study the transport properties (particle, photon) of multifractals and compare the results with the homogeneous plane parallel situation. Since the plane parallel and multifractal radiative properties diverge for increasingly thick clouds, it becomes fundamentally important to characterize the scaling properties and optical thickness of real clouds.