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Numerically simulated three-dimensional tropical convective systems were analyzed using a wavelet approach in which the vertical shear of the ambient wind is used as a decomposition criterion. The method objectively decomposes the simulated systems into their two primary components, namely organized deep convection and a mesoscale stratiform region. This reproduces the standard model of highly organized mesoscale convective systems as well as giving an objective characterization of less organized regimes. It demonstrates the vertical component of wind shear as a statistically useful criterion in addition to its better known role as a quasi-deterministic mechanism controlling the organization of convection and its scale selection.

Wavelet Analysis of Simulated Tropical Convective Cloud Systems. Part II: Decomposition of Convective-Scale and Mesoscale Structure