The dynamics of the Changma rains in the early summer, which derive from baroclinic disturbances that are strongly modified by latent heat release, remain poorly understood.
2.
The full development of a medicane often necessitates the formation of a large-scale baroclinic disturbance transitioning late in its life cycle into a tropical cyclone-like system, nearly always under the influence of a deep, cut-off, cold-core low within the middle-to-upper troposphere, frequently resulting from abnormalities in a wide-spreading Rossby wave massive meanders of upper-atmospheric winds.
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