Cyclones begin life as tropical low-pressure systems.
Tropical lows form over warm water (at least 26.5°C). Over warm oceans, a tropical low draws up warm, moist air from the sea. As this air rises and meets cooler air above, it condenses into dense storm clouds. These clouds form around the low-pressure system and begin to spin or rotate. As they spin, they draw in more moist, warm air causing the system to grow.
As air moves towards the centre of the tropical low, it speeds up and increases in strength. This pulls more air into the system, making the cyclone stronger.
If cool air sinks into the centre of the low-pressure system, it creates the relatively calm area called the eye. The eye can be 10-100 km wide. It is surrounded by a wall of thunderstorms and strong winds.
Tropical lows officially become cyclones when wind speeds are greater than 63km/h. They will then receive a name from the Bureau of Meteorology. Naming helps to reduce public confusion, especially in the event of multiple simultaneous cyclones.