How does Earth tilt affect climate

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The Earth's axial tilt, also known as obliquity, is the angle at which the Earth's axis is tilted relative to its orbit around the Sun. This tilt has a significant impact on the climate of different regions on Earth.

The tilt of the Earth's axis is responsible for the changing seasons. When a particular hemisphere is tilted towards the Sun, it receives more direct sunlight and experiences warmer temperatures, leading to summer. Conversely, when that hemisphere is tilted away from the Sun, it receives less direct sunlight and experiences colder temperatures, leading to winter.

The tilt also affects the distribution of sunlight across the Earth's surface, resulting in variations in day length and the angle at which sunlight hits the Earth's surface. This can influence the intensity and duration of seasons, as well as the amount of solar energy absorbed by different regions.

Overall, the Earth's tilt plays a crucial role in shaping the climate patterns and seasons that we experience on a global scale. It is one of the key factors that contribute to the diversity of climates and ecosystems found on Earth.
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