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Short wavelength radiation such as Ultraviolet fall to absorption spectrum band of Ozone. Ozone absorb UV and re-emitted the radiation in the range of infrared or thermal range radiation.
The radiation emitted by the Earth peaks around 10 microns, whereas that from the sun peaks under 1 micron. This is why Earth's radiation is referred to as longwave and solar radiation as shortwave, commonly. All objects emit radiation because all objects have a temperature. In fact, using Wien's Law you can very simply calculate the wavelength, lambda, of maximum emission: lamda(max) = c/T where c is a constant (2897) and T is the temperature of the emitting surface in Kelvin.
The sun heats the atmosphere. Solar radiation largely passes through the atmosphere and warms the surface of the earth. The earth then radiates heat up into the lower levels of the atmosphere where greenhouse gases warm. The warmed greenhouse gases then continue to radiate heat in all directions warming the atmosphere and again the earth's surface.
Energy is re-radiated by the Earth as infrared (thermal) radiation.
90% of radiation reaching the surface of the earth is absorbed! and 10% is reflected into space.
they are longer than those emitted by the sun.
Terrestrial radiation refers to heat emitted from the earth's atmosphere and surface.
Heat rises from the surface of the earth in the form of infra-red radiation.
Not as ultraviolet; the radiation is emitted as infrared radiation.
Water vapor.
From the surface. Solar radiation is absorbed by the surface and emitted at a longer wavelength, which is essentially heat.
In the core of the star, the heat then spreads out to the surface and is emitted as EM radiation
The magnitude of the incident angle with the normal of the reflection surface and reflection angle with the normal of the surface are the same. The direction of the reflection is away form the surface and the incident is toward the surface.
water vapor and carbon dioxide.
If you were to measure reflected radiation then you would be measuring the temperature of the source of light (the sun)! So you need to look at the emmited radiation (measured during the night) to guage the temperature of the ocean's surface.
Because the Sun is the primary source of all energy in the Solar System.The effective surface temperature of the Sun is 5,778 KelvinEnergy received by Earth will be radiated back into space, both during the day and at night. The average temperature on Earth is such, that the amount of radiation received, and the amount of radiation emitted, is in equilibrium (on average).
Short wavelength radiation such as Ultraviolet fall to absorption spectrum band of Ozone. Ozone absorb UV and re-emitted the radiation in the range of infrared or thermal range radiation.