Final answer:
The key factor for cyclogenesis and the growth of low pressure systems is a strong Coriolis force, which influences the rotation and intensity of cyclones, contributing to their development.
Step-by-step explanation:
One of the biggest keys for cyclogenesis and the intensification of a low-pressure system is a strong Coriolis force. The Coriolis force affects the rotation direction of cyclones, causing them to rotate counterclockwise in the Northern Hemisphere and clockwise in the Southern Hemisphere.
This rotation is part of what characterizes these storm systems, which include hurricanes, typhoons, and tropical storms, all of which are accompanied by low-pressure centers, strong winds, and heavy rains.
Air flowing towards a region of low pressure in a tropical cyclone will be deflected, contributing to the rotation and intensification of the storm system, as well as the cooling and cloud formation that make these low-pressure systems visible from space. A large difference in atmospheric pressure between two areas is also crucial for the development and intensification of storms.