The traditional four-season cycle (Spring, Summer, Autumn, Winter) is primarily a phenomenon of . In other parts of the world, seasonality takes different forms:
Near the equator, temperature varies little. Instead, seasons are defined by rainfall, resulting in Wet (Monsoon) and Dry seasons .
The traditional four-season cycle (Spring, Summer, Autumn, Winter) is primarily a phenomenon of . In other parts of the world, seasonality takes different forms:
Near the equator, temperature varies little. Instead, seasons are defined by rainfall, resulting in Wet (Monsoon) and Dry seasons .