Scale Invariance, Symmetries, Fractals, and Stochastic Simulations of Atmospheric Phenomena

Abstract

Advances in remote sensing and in situ measurement techniques have revealed the full continuum of atmospheric motions and have underlined the importance of mesoscale processes. This paper examines the implications of three observed characteristics of mesoscale circulations: 1) the energy spectrum of the horizontal wind in the horizontal is of the form k"ft with fa ~ 5/3, (k is a wavenumber); 2) the corresponding spectrum in the vertical direction is of the same scaling form, but with a very different slope (fa ~ 11/5); and 3) the variability is extreme.