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Air can rise in one of four ways:
1) Orographic Lifting
- air travels up the side of the mtn
2) Frontal Wedging
- cold, dense air acts a wedge for warm. less dense air to rise on
3) Convergence
- two air masses come together, little difference in temp or density--> "collide", energy has to go somewhere--> air is forced upward
4) Localized Convective Lifting
- uneven heating of Earth by sun--> pockets of warm air that rise up
* As the air rises upward, it cools adiabatically until it reaches the dew point, at which point the air condenses into a cloud. Once the cloud becomes saturated with water, it rains. *
What else can I help you with?
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