The Horizontal Movement Speed of Cumulus Clouds in a Shear Flow : A Two-Dimensional Numerical Experiment

Cumulus clouds in a shear flow are simulated by a two-dimensional slabsymmetric model with two different finite-difference schemes. It is known that the horizontal speed of the top of simulated clouds is less than the ambient wind speed at that height. This is explained in the developing stage by the transformation of the circulation pattern arising from vertical wind shear and in the dissipating stage by the asymmetrical distribution of liquid water content arising from the transformation of circulation.