Seasonal reversal of wind patterns (e.g., Indian monsoon) arises from differential heating of land and ocean. Summer heating over continents creates low-pressure systems that draw moisture-laden air from oceans, producing heavy rainfall.
If you are building this as a developer, here is how you generally structure the logic: yearly seasons
Earth’s axis remains fixed in space (pointing toward Polaris) as the planet orbits the Sun. During one half of the year (March to September), the Northern Hemisphere tilts toward the Sun, receiving more direct solar radiation and longer days—producing summer. Simultaneously, the Southern Hemisphere tilts away, experiencing winter. The opposite occurs from September to March. Seasonal reversal of wind patterns (e
The yearly seasons are caused by the tilt of the Earth's axis (approximately 23.5 degrees) and its orbit around the Sun. As the Earth rotates on its axis, it also revolves around the Sun in an elliptical path. The tilt of the axis causes the amount of sunlight that reaches the Earth's surface to vary throughout the year, resulting in the changing seasons. During one half of the year (March to
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