TYPES OF CYCLONE
(1) Hurricanes in north America 
(2) The Caribbean , typhoons in eastern Asia 
(3) The cyclones in India
when warm, moist air over the ocean rises upward from near the surface, a cyclone is formed. When the air rises up and away from the ocean surface, it creates an area of lower air pressure below. The difference of temperature between the warm, rising and the cooler environment causes the air to rise and become buoyant.
Polar cyclones (also known as Arctic Cyclones) are large areas of low pressure. Polar cyclones are usually 1,000 to 2,000 kilometers wide in which the air is moving in a spiral counterclockwise fashion in the northern hemisphere. The reason for the rotation is the same as tropical cyclones, the Coriolis effect.
A mesocyclone is storm-scale region of rotation (vortex), typically around 2 to 6 mi (3.2 to 9.7 km) in diameter, most often noticed on radar within thunderstorms. In the northern hemisphere it is particularly found in the right rear flank of a supercell, or often on the eastern, or leading, flank of a storm with heavy downpour. 
An extratropical cyclone (also called a mid-latitude cyclone) is a type of cyclone. It is a large low-pressure weather area with clouds, rain and heavy wind. They occur in areas that are between latitudes 30° – 60° from the equator. These cyclones are usually connected with fronts.

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