All the above
All answers are correct.
The darkness or lightness by itself doesn't affect the heat capacity, only how easily radiation will be absorbed - and emitted.The darkness or lightness by itself doesn't affect the heat capacity, only how easily radiation will be absorbed - and emitted.The darkness or lightness by itself doesn't affect the heat capacity, only how easily radiation will be absorbed - and emitted.The darkness or lightness by itself doesn't affect the heat capacity, only how easily radiation will be absorbed - and emitted.
Radiation is absorbed maily because of resonance.
A unit of absorbed radiation is called a gray (Gy).
This Answer is as Variable, considering all of the varying Parameters, as it is Crucial to Our Tenuous Situation. This percentage, as Critical as it is, in not predictable as the Output of Solar radiation is as unknowable as the powerful Incidence of detrimental Cosmic Rays.
Yes, radiation can be absorbed by a silver surface. The absorption of radiation will depend on factors such as the type of radiation, the energy level, and the thickness of the silver surface.
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.
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.
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 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.
Approximately 51% of incoming solar radiation is absorbed by Earth's surface. The rest is reflected back into space or absorbed by the atmosphere.
The radiation emitted by a body that absorbed it first is known as re-emitted or secondary radiation. This occurs when absorbed energy is re-radiated by the object in a different form such as heat or light.