1. Strong upward movement of air draws water vapour up from the warm ocean surface
2. This evaporated air cools as it rises and condenses to form towering thunderstorm clouds
3. As the air condenses it releases heat which powers the storm and draws up more and more water from the ocean
4. Several smaller thunderstorms join together to form a giant spinning storm
5. When surface winds reach an average of 120km per hour (75 miles per hour) the storm officially becomes a tropical storm
6. The storm now develops an eye at its centre where air descends rapidly. The outer edge of the eye is the eyewall where the most intense weather conditions (strong winds and heavy rain) are found
7. As the storm is carried across the ocean by the prevailing winds, it continues to gather strength
8. If the storm reaches warm seas after crossing the land, it may pick up strength again
9. On reaching land the storm's energy supply (evaporated water) is cut off. Friction with the land slows it down and it begins to weaken