Thunderstorms are a result of the tropical climate with high temperatures and humidity make the climate instability. (instability), or the atmosphere have not stabilized the mixed compound from the bottom upwards. And from the top downwards. In the first stage, air or atmosphere flow more strongly (strong convective updraft) and Next, which is the decomposition (dissipating stage) to the air stream flowing into severe (strong downdraft) in column (a) of rain. thunderstorms are frequent formation of up to 40,000 to 50,000 feet in the middle latitudes (mid - latitude) and higher than in the tropics. The lower layers of the atmosphere, stratosphere sphere of stability is very good (great stability) can only inhibit the formation of a thunderstorm possible
in thunderstorms meteorological divided into several types. Depending upon the nature of the weather, such as thunderstorms and air (air - mass thunderstorm) clouds in the Squash Club (squall - thunderstorm) clouds and the air resistance levels (frontal thunderstorm).
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