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In many countries, people talk about four distinct seasons: spring, summer, autumn and winter. But in several parts of India and other tropical regions, people mostly talk about just summer, monsoon and maybe a short winter. Why is there such a difference in seasonal patterns across the world?

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The main reason for different seasonal patterns is the tilt of the Earth’s axis and a region’s distance from the equator. Countries in the temperate zones, such as Europe and North America, are far from the equator. As the Earth orbits the Sun, these regions receive varying amounts of sunlight across the year, creating four distinct seasons—spring, summer, autumn and winter.

In contrast, regions near the equator and in the tropics receive more consistent sunlight throughout the year. Here, the main changes are between wet (rainy) and dry seasons, rather than extreme hot and cold differences.

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In India, for example, the climate is strongly influenced by the monsoon winds. So we often describe seasons as summer, monsoon and winter. However, in high-altitude areas like the Himalayas, seasonal changes are more similar to temperate regions. For exam purposes, remember: seasons depend on Earth’s tilt, revolution around the Sun and latitude of the place. This concept is very important in basic geography.

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