Formation of a tropical storm
1. Warm, moist air rises, leaving an area of low pressure below
2. Warm air from surrounding areas of higher pressure moves into this low pressure area and rises too
3. Warm air cools, condensing into thunderstorm clouds
4. The whole system is spinning due to the Coriolis effect
5. Constant additions of energy from the warm air causes the storm to spin faster and generate higher wind speeds
6. Eye of the storm is an area of extremely low pressure with cool, dry air descending
7. Surrounding the eye is the eyewall, the most intense and powerful area of the storm
8. When the tropical storm reaches a coast, the low pressure and high winds will cause a storm surge
9. When the storm reaches land, the eye eventually collapses and heavy rain can persist for days