Ozone layer protects the earth from the dangerous ultra violet radiations of the sun. It is present in the stratosphere region of the atmosphere.
The type of radiation that can be observed well from Earth's surface is primarily visible light, which is part of the electromagnetic spectrum. This range of wavelengths is not significantly absorbed by the atmosphere, allowing us to see sunlight and other light sources. Additionally, some radio waves can also be detected from the surface, although certain frequencies may be affected by atmospheric conditions. Other types of radiation, such as ultraviolet and X-rays, are largely absorbed by the atmosphere and are not easily observed from the ground.
no
Electromagnetic energy that enters the Earth's atmosphere can be reflected back into space or absorbed by the atmosphere and surface. Absorption can lead to heating of the atmosphere and contribute to processes like the greenhouse effect.
Ozone layer protects us. It is present in the stratospheric region of atmosphere.
Ozone layer protects us from harmful radiations. UV radiations are these rays.
it bounce back the UV radiations
Ozone layer protects us from the harmful UV radiations of the sun. It filters out these harmful radiations. It is present in stratosphere.
Earth's energy is solely infrared energy.
Earth's ozone layer is a protective one. It protects from UV radiations.
absorbed
Ozone layer protects the earth from the dangerous ultra violet radiations of the sun. It is present in the stratosphere region of the atmosphere.
Ultraviolet, visible light, and some radio waves are able to penetrate the Earth's atmosphere. However, X-rays and gamma rays are largely absorbed and blocked by the atmosphere.
Yes, microwave radiation can pass through the Earth's atmosphere. However, not all microwave frequencies can pass through easily, as some are absorbed by water vapor and other gases in the atmosphere. This is why certain frequencies are used for applications such as satellite communication and radar systems.
The type of radiation that can be observed well from Earth's surface is primarily visible light, which is part of the electromagnetic spectrum. This range of wavelengths is not significantly absorbed by the atmosphere, allowing us to see sunlight and other light sources. Additionally, some radio waves can also be detected from the surface, although certain frequencies may be affected by atmospheric conditions. Other types of radiation, such as ultraviolet and X-rays, are largely absorbed by the atmosphere and are not easily observed from the ground.
About 50% of the sun's radiation that reaches Earth's atmosphere is absorbed by the Earth's surface. The remaining energy is either reflected back to space or absorbed by the atmosphere.
no