How do tropical storms form?
- 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.
friction slows it down and it begins to weaken