Atmospheric stability and instability
1. Parcels of hot air rise, expand and cool, becoming less dense
2. Rate of cooling is less if water vapour in the air mass starts to condense
3. If the air parcel is warm enough there are a high number of collisions, and the water remains in gas form
4. As the air mass expands and the number of collisions reduces the amount of heat reduces, and water vapour drops back into water form
5. Each time a change occurs, such as gas to solid there is energy produced