1. Angle of sunlight: affected by latitude, seasons, and local topography. Sunlight has to pass through more atmosphere near the poles, fewer photons per land area.
2. Global wind patterns: rooted in points at the equator moving much faster than points near the poles during the earth's revolution
- a residual effect of displaced air is wind, can be strong at the poles and the equator
- ascending moist air causes lots of rainfall near equator
- descending dry air at 30 degrees latitude leads to deserts
3. Mountains: has significant effect on the amount of sunlight that reaches an area, local temperature and rainfall patterns
- uplifted air cooling and dropping all moisture on the
windward side of mountains. This leaves only dry air once it
descends on the leeward side of the mountain range, which
LEADS TO RAIN SHADOW