We do not have your graph and can't answer. I would suggest you look at the graphs and the vectors.
Most of the radiation absorbed in Earth's atmosphere is absorbed in the ozone layer, which is a region of the stratosphere that contains a high concentration of ozone molecules. Ozone absorbs ultraviolet radiation from the sun, protecting life on Earth from its harmful effects.
No, not all the radiation absorbed in the Earth's atmosphere is absorbed in the stratosphere. Different layers of the atmosphere absorb different amounts of radiation. The stratosphere mainly absorbs ultraviolet radiation, while other layers like the troposphere absorb various wavelengths of radiation as well.
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.
Approximately 70% of the solar radiation that arrives at the top of the Earth's atmosphere is absorbed by the Earth's surface, while the remaining portion is reflected back into space or absorbed by the atmosphere.
Approximately 51% of incoming solar radiation is absorbed by Earth's surface. The rest is reflected back into space or absorbed by the atmosphere.
Most of the radiation absorbed in Earth's atmosphere is absorbed in the ozone layer, which is a region of the stratosphere that contains a high concentration of ozone molecules. Ozone absorbs ultraviolet radiation from the sun, protecting life on Earth from its harmful effects.
The amount of ozone in atmosphere determine s the % of solar radiation that will be absorbed. The absorbtion of radiation is proportional to the concentration of ozone.
No, not all the radiation absorbed in the Earth's atmosphere is absorbed in the stratosphere. Different layers of the atmosphere absorb different amounts of radiation. The stratosphere mainly absorbs ultraviolet radiation, while other layers like the troposphere absorb various wavelengths of radiation as well.
No, not all radiation absorbed in the Earth's atmosphere is absorbed in the stratosphere. Different layers of the atmosphere absorb different types of radiation. For example, the ozone layer in the stratosphere absorbs a significant amount of ultraviolet radiation, but other layers like the troposphere also absorb certain wavelengths of radiation.
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.
Approximately 70% of the solar radiation that arrives at the top of the Earth's atmosphere is absorbed by the Earth's surface, while the remaining portion is reflected back into space or absorbed by the atmosphere.
Some is absorbed by molecules in the atmosphere (such as ultraviolet absorption by ozone), some is absorbed on the surface, and some is reflected by clouds or the surface back into space. The surface will re-radiate much of the absorbed solar radiation as infrared (thermal) radiation, and some of this is then absorbed by atmospheric gases such as carbon dioxide and methane.
Gases can absorb radiation, where specific gases like water vapor, carbon dioxide, and methane can trap heat in the atmosphere, contributing to the greenhouse effect and global warming. Gases can also scatter radiation, leading to phenomena like Rayleigh scattering in the atmosphere, which is responsible for the blue color of the sky.
Atmosphere continuously receives radiation. Some like UV are absorbed by ozone.
Greenhouse!
Radiation directed at Earth can be absorbed or scattered by the atmosphere before reaching the surface. Different types of radiation can interact with particles in the atmosphere, causing them to be reflected, absorbed, or scattered in different directions, preventing them from reaching the Earth's surface in full intensity.
Approximately 51% of incoming solar radiation is absorbed by Earth's surface. The rest is reflected back into space or absorbed by the atmosphere.