It is usually known as a cyclone with intense winds that are accompanied by storms with heavy rain, although it is also assigned to areas or areas of the world where the atmospheric pressure is quite low. The word "cyclone" was used for the first time in 1840 by Henry Piddington.
The development or formation of a low pressure system is called Cyclogenesis and it is a term made up of several similar processes that give rise to the development of a certain class of cyclone and can occur at any of the scales managed in meteorology (microscale and synoptic scale) less on the planetary scale.
There are different types of cyclones, however, some of them will be named below:
Tropical Cyclones: also known as tropical storms, hurricanes and typhoons, generally formed in hot oceans, sucking the energy of evaporation and condensation. They originate from the formation of centers of low atmospheric pressure within the sea.
Extratropical cyclones: they are formed by latitudes greater than 30 ° and are composed of two or more air masses, the variety of cyclones of this type is wide and the identification of a subfamily of this type is still in process.
Subtropical cyclones: meteorological system that has characteristics similar to the tropical cyclone as well as the extratropical cyclone and usually form in latitudes close to the equator.
Polar cyclones are similar and the size of tropical cyclones, although they are very short-lived. Unlike other cyclones, this one develops extreme speed and reaches a maximum of 24 hours of force.
Finally, the mesocyclones: these emit a layered rotation inertia appearing in the form of a cloud, which allows it to increase its rotation, forming a tornado.