Air is heated which rises rapidly, which draws in more air and large volume of moisture from the ocean. This causes strong winds.
The rising air starts to cool and condense forming clouds. This releases latent heat, which powers the tropical storm.
The winds will start to spiral into the storms eye, due to the coriolis effect. This causes the colder, dry air to sink into the eye, causing the calm conditions in the eye.
The storm continues to expand it reaches land, which causes friction, which slows it down, and it loses its power source.