Hot, wet air rises and expands and cools as it rises, forming clouds where water condenses and causes precipitation. It tries to equilibrate by going to the poles as there is less energy there on average. As it goes, it will begin to cool, and descend as cool, dry air.
- A strong upward movement of air draws water vapour up from the warm ocean suface (27 degrees +)
- This evaporated air cool as it rises and forms thunderstorm clouds
- As the air condenses it releases heat which powers the storm and draws up more water
- Several smaller thunderstorms join together to form a giant spiralling storm
- when surface winds reach an average of 120km the storm becomes a tropical storm
- the storm now develops an eye at its centre where air descends rapidly. the outer edge of the eye is the eyewall which has the most intense weather conditions
- the storm gathers strength as it is carried across the ocean
- upon reaching land the storm's energy supply (evaporated water) is cut off.