Seasons are the result of the Earth's axial tilt and its orbit around the Sun. The Earth's axis is tilted at an angle of approximately 23.5 degrees relative to its orbital plane. This tilt causes the amount of sunlight received at different latitudes to vary throughout the year, leading to the changing of seasons.
As the Earth orbits the Sun, the tilt of its axis causes different parts of the Earth to receive varying amounts of sunlight at different times of the year. When a particular hemisphere is tilted towards the Sun, it experiences summer, while the opposite hemisphere, tilted away from the Sun, experiences winter. This is what causes the cycle of seasons.
The changing seasons have a significant impact on climate, weather patterns, and ecological processes. For example, during summer, the increased sunlight and longer days lead to warmer temperatures and the growth of plants. In contrast, winter brings colder temperatures, shorter days, and in some regions, snowfall.
Here are some key points to understand about the seasons:
By understanding the causes and effects of seasons, you can gain insight into the interconnectedness of Earth's systems and the profound influence of astronomical phenomena on our daily lives.
.