Cyclonic Rainfall

Cyclonic Rainfall

Cyclone is the specific air formation when the pressure at an area is less than the surrounding regions. 

It is formed when two masses of air of different temperature, humidity, and density meet. Warm air and cool air do not mix as they have different densities. The warm air rises over the heavier cool air. 

Warm air from the surrounding regions comes to the centre of the cyclone and starts moving upward. 

As it rises, the temperature of the air reduces. Then condensation occurs resulting in cyclonic rainfall. 

They are cyclonic and stormy in nature.