ABSTRACT
A hurricane in a formative stage often does show separate centers, a thought process for the formation of a hurricane that can start from such an idea. The thunderstorm forming over the tropical ocean is an initial step toward reducing the lack of equilibrium between the sea level humidity and enthalpy and their values in the upper atmosphere, which was quoted earlier as representing an energy cost of 100 MJ/m2. So, conceptually, thunderstorms are arranged in a ring of variable radius. If the ring radius is very large, there will be scarcely any effect; each storm will simply have two neighbors and will pull in air from the surrounding sea surface to pump upwards. The conventional description of the hurricane is of a primary azimuthal airflow, the sea-level hurricane wind, and the secondary in-, up-, and out-flow that is more like the thunderstorm flow.
