The atmoshere can stop the gamma ray but the half of the atmosphere that gets hit by the gamma ray will be destroyed. Chemicals in the gamma ray will eat the ozone and destroy the atmosphere leaving the earth unprotected against the suns U-V rays.
Roughly 20% of visible light radiation is absorbed as it passes through the Earth's atmosphere. The remaining percentage is either reflected back into space or reaches the Earth's surface. This absorption is influenced by factors such as cloud cover, aerosols, and gases in the atmosphere.
Visible light passes through the atmosphere primarily because it consists of wavelengths that are not significantly absorbed or scattered by the gases and particles present in the air. Unlike ultraviolet or infrared radiation, which can be absorbed by ozone or water vapor, visible light interacts minimally with atmospheric constituents. This allows it to reach the Earth's surface, enabling us to see and support photosynthesis in plants. Additionally, the atmosphere's transparency to visible light is crucial for maintaining the planet's energy balance.
When visible light enters Earth's atmosphere, it interacts with air molecules and scatters in different directions. Some of the light is absorbed by gases like ozone and water vapor, while the rest continues through the atmosphere and reaches the surface of the Earth, enabling us to see our surroundings.
The atmosphere is mostly transparent at the frequencies of visible light; in fact, the fact that our eyes see in that range is probably BECAUSE it is the transparent frequency range.Light that hits the atmosphere will predominantly penetrate the atmosphere and reach the Earth. Some small percentage of the light will be absorbed or scattered passing through, and a very small percentage will be reflected and bounce back into space.
Red light from the sun is scattered by the Earth's atmosphere during the day, making it less visible in the sky. At sunrise and sunset, the sunlight has to pass through more of the atmosphere, scattering shorter-wavelength colors and allowing the longer-wavelength red light to be more visible in the sky.
Roughly 20% of visible light radiation is absorbed as it passes through the Earth's atmosphere. The remaining percentage is either reflected back into space or reaches the Earth's surface. This absorption is influenced by factors such as cloud cover, aerosols, and gases in the atmosphere.
The atmosphere is transparent to the visible light of the Sun. So it passes right through, only to get absorbed by the surface of the Earth.
The Earth and atmosphere absorb the visible and infrared energy and this warms the earth.
The Earth's atmosphere is most transparent to visible light, particularly within the wavelengths of red, green, and blue. These wavelengths pass through the atmosphere with minimal absorption or scattering, allowing us to see objects clearly.
almost none the vast majority of visible light passes through the atmosphere.
That is transferred mainly through visible and infrared light.That is transferred mainly through visible and infrared light.That is transferred mainly through visible and infrared light.That is transferred mainly through visible and infrared light.
Earth's atmosphere is mostly transparent to visible light, radio waves, and some portions of the infrared and ultraviolet spectra. This allows these forms of light energy to reach the surface of the Earth relatively unimpeded.
Visible light passes through the atmosphere primarily because it consists of wavelengths that are not significantly absorbed or scattered by the gases and particles present in the air. Unlike ultraviolet or infrared radiation, which can be absorbed by ozone or water vapor, visible light interacts minimally with atmospheric constituents. This allows it to reach the Earth's surface, enabling us to see and support photosynthesis in plants. Additionally, the atmosphere's transparency to visible light is crucial for maintaining the planet's energy balance.
When visible light enters Earth's atmosphere, it interacts with air molecules and scatters in different directions. Some of the light is absorbed by gases like ozone and water vapor, while the rest continues through the atmosphere and reaches the surface of the Earth, enabling us to see our surroundings.
Energy from the sun reaches the Earth through electromagnetic radiation, primarily in the form of visible light. This light travels through the vacuum of space and reaches the Earth's atmosphere, where it is absorbed and converted into heat energy.
Infra red and visible light.
The atmosphere is mostly transparent at the frequencies of visible light; in fact, the fact that our eyes see in that range is probably BECAUSE it is the transparent frequency range.Light that hits the atmosphere will predominantly penetrate the atmosphere and reach the Earth. Some small percentage of the light will be absorbed or scattered passing through, and a very small percentage will be reflected and bounce back into space.