Seasonal Changes

Seasonal changes refer to the variations in climate and environmental conditions that occur in a predictable pattern throughout the year due to the tilt of the Earth’s axis and its orbit around the sun. These changes are marked by distinct seasons—typically spring, summer, autumn (fall), and winter—each characterized by unique weather patterns, temperatures, and daylight hours.

During spring, temperatures begin to rise, leading to the blooming of plants and the awakening of wildlife. Summer is characterized by warm or hot temperatures and longer days. Autumn sees a cooling period, with many trees shedding their leaves as they prepare for winter. Finally, winter brings colder temperatures, potential snowfall, and shorter days, often resulting in dormancy in many plant and animal species.

These shifts not only affect the weather but also influence ecosystems, agriculture, and human activities such as festivals and holidays that are often tied to specific seasons. Seasonal changes are fundamental to the natural world, driving cyclical processes and adaptations in plants, animals, and humans alike.