There are several factors that contribute to the differences in the distribution of solar energy on Earth's surface. These include:
1. Latitude: Solar energy is more concentrated near the equator compared to the poles. This is because sunlight hits the Earth's surface at a more direct angle near the equator, leading to higher solar radiation and energy.
2. Earth's tilt and rotation: The Earth's tilt and its rotation around the sun create seasons. During summer in the hemisphere tilted towards the sun, solar energy is more intense and the days are longer. In contrast, during winter in the hemisphere tilted away from the sun, solar energy is less intense, and the days are shorter.
3. Atmospheric conditions: The Earth's atmosphere plays a role in the distribution of solar energy. The atmosphere absorbs and scatters sunlight, leading to variations in solar energy reaching the surface. Areas with less atmospheric interference, such as deserts, receive more direct sunlight and thus have higher solar energy.
4. Topography: The Earth's surface features, such as mountains and valleys, affect the distribution of solar energy. Mountains can block sunlight and create shadows, resulting in lower solar energy in certain areas. On the other hand, valleys or flat areas can capture and concentrate solar energy.
5. Cloud cover and weather patterns: Cloud cover and weather patterns vary across the Earth's surface, greatly influencing solar energy distribution. Clouds can reflect and absorb sunlight, reducing the amount of solar energy reaching the surface. Areas with frequent cloud cover may have lower solar energy availability compared to areas with clearer skies.
Overall, these factors contribute to the differences in solar energy distribution on Earth's surface, leading to varying levels of solar radiation and energy received in different regions.
Which explains in the differences in the distribution of solar energy on Earths surface
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