It can go out to space, or it can be trapped by various gases in the atmosphere, i.e., greenhouse gases such as CO2 and water vapor.
When radiation reaches Earth's surface, it can be absorbed, reflected, or scattered. The amount of radiation that is absorbed can contribute to heating of the surface and atmosphere. This process is fundamental for maintaining Earth's energy balance and climate.
As radiation passes through Earth's atmosphere, some of it is absorbed and scattered by gases and particles. This can result in attenuation of the radiation, meaning that its intensity decreases. Different types of radiation are affected in various ways based on their energy and wavelength.
Incoming solar radiation that is reflected off the surface of the Earth can be absorbed by atmospheric gases, clouds, or particles in the air. Some of this radiation can be scattered or absorbed by the atmosphere and re-emitted as infrared radiation. This process helps regulate the Earth's temperature and maintain the energy balance of the planet.
The atmosphere helps to balance the unequal heating of Earth's surface by redistributing heat through convection and wind patterns. This process involves transferring heat from warmer areas to cooler areas, helping to regulate temperature across the globe. The atmosphere also absorbs and reemits solar radiation, which further contributes to stabilizing Earth's temperature.
The most common radiation on Earth is non-ionizing radiation from the sun, such as visible light, infrared radiation, and ultraviolet radiation. These forms of radiation are generally low in energy and do not have enough power to ionize atoms or molecules.
Most of the solar radiation is absorbed when it reaches the surface of the earth. Some of the solar radiation is also absorbed in the atmosphere.
More radiation reaching the Earth's surface.
Radiation.
It is absorbed.
The shortwave radiation that reaches Earth's surface and is not reflected is absorbed by the surface, warming it up.
As the sun's rays heat up the earth, the radiation hits the atmosphere. Then the radiation heads back to the sun.
When radiation reaches Earth's surface, it can be absorbed, reflected, or scattered. The amount of radiation that is absorbed can contribute to heating of the surface and atmosphere. This process is fundamental for maintaining Earth's energy balance and climate.
Earth is exposed to the dangerous radiation of the sun.
Some of the radiation not absorbed by the Earth is reflected back into space by the atmosphere, clouds, and the Earth's surface. The remaining portion may be scattered in different directions or absorbed by gases in the atmosphere.
UVC radiation is absorbed by the ozone layer in the Earth's atmosphere, preventing it from reaching the Earth's surface. If UVC radiation were to reach the surface, it can be harmful to living organisms as it can damage genetic material and cause skin cancer.
As radiation passes through Earth's atmosphere, some of it is absorbed and scattered by gases and particles. This can result in attenuation of the radiation, meaning that its intensity decreases. Different types of radiation are affected in various ways based on their energy and wavelength.
It find its way to earth