Tropical storms form from an atmospheric disturbance just like a tropical wave or team of thunderstorms. For these disturbances to mature right into a tropical cyclone, the subsequent environmental conditions need to be in place:
A tropical cyclone is usually a rotating small-tension weather conditions process which has arranged thunderstorms but no fronts (a boundary separating two air masses of different densities). Tropical cyclones with optimum sustained surface winds of less than 39 miles for every hour (mph) are termed tropical depressions.
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