The Sun light is not monochromatic.
If Earth were flat, the distribution of thermal energy would likely differ due to the altered surface area and angle of incidence of solar radiation. The regions near the center of the flat Earth would receive more direct sunlight and experience higher temperatures, while the edges would receive less sunlight and be cooler. This could lead to more extreme temperature variations across the flat Earth compared to the current spherical Earth.
On a yearly basis the Earth receives the same amount of sunlight on its total surface. The distribution of light to dark periods is different by latitude and time of year
Materials on Earth typically absorb shorter wavelengths of electromagnetic energy compared to the wavelengths they radiate. This is because materials absorb higher energy radiation (such as ultraviolet or visible light) and emit lower energy radiation (such as infrared or thermal radiation).
The Earth receives varying amounts of sunlight due to its spherical shape and tilted axis. This tilt causes different parts of the Earth to receive direct sunlight at different angles, leading to variations in the amount of sunlight received. Factors like seasons and Earth's orbit around the sun also affect the distribution of sunlight on Earth's surface.
Here on earth it is violet wavelengths that scatter the most, however the earth's sun emits more blue light than violet so blue wavelengths are scattered more frequently than violet wavelengths.
The sun emits various types of electromagnetic radiation, but the majority of the radiation that reaches Earth's surface is in the form of visible light. This includes wavelengths that range from ultraviolet to infrared.
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The Earth's atmosphere acts like a filter, allowing certain wavelengths of light to pass through while absorbing or reflecting others. Wavelengths such as ultraviolet and X-ray radiation are absorbed by gases like ozone and oxygen in the atmosphere, protecting life on Earth from harmful radiation. This selective filtering ensures that only specific wavelengths necessary for life and the environment reach the Earth's surface.
God created the earth. He didn't have to receive it because it was his.
Most of the sun's energy is emitted as light in various wavelengths. Earth receives only a small fraction of this energy because it's located at a significant distance from the sun. Also, Earth's atmosphere scatters and absorbs some of the incoming solar radiation.
The ozone protects life on earth by absorbing certain wavelengths of ultraviolet radiations. These radiations are high frequency radiations which can cause serious harm to living organisms.