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Absorption (electromagnetic radiation)
From Wikipedia, the free encyclopedia
In physics, absorption is the process by which the energy of a photon is taken up by another entity, for example, by an atom whose valence electrons make transition between two electronic energy levels. The photon is destroyed in the process. The absorbed energy may be re-emitted as radiant energy or transformed into heat energy. The absorption of light during wave propagation is often called attenuation.
The absorbance of an object quantifies how much light is absorbed by it (not all photons get absorbed, some are reflected or refracted instead). This may be related to other properties of the object through the Beer-Lambert law.
For most substances, the amount of absorption varies with the wavelength of the light, leading to the appearance of colour in pigments that absorb some wavelengths but not others. For example, an object that absorbs blue, green and yellow light will appear red when viewed under white light. More precise measurements at many wavelengths allow the identification of a substance via absorption spectroscopy.
The specific phenomena involving absorption of electromagnetic radiation at the Earth's surface have several important aspects. These phenomena include regulating the temperature of the Earth's crust, surface waters and lower atmosphere. Changes in the Earth's crust such as glaciation, deforestation, polar ice melting, will necessarily alter the quantity and wavelength selectivity of electromagnetic absorption at the Earth's surface; correspondingly, changes in climate such as global warming may accompany changes in electromagnetic absorption or its inverse, the albedo.[1][2] Regulation of the temperature of surface waters has been analyzed with respect to the influence of electromagnetic radiation absorption, indicating the effects of total solar insolation and the local albedo.[3][4]
- ^ Department of Physics & Astronomy. Relationship of Albedo to Global Warming. Georgia State University. Retrieved on 2007-03-06.
- ^ Wielicki, Bruce A.; Wong, Takmeng; Loeb, Norman; Minnis, Patrick; Priestley, Kory; Kandel, Robert (6 May 2005). "Changes in Earth's Albedo Measured by Satellite". Science 308 (5723): 825. doi:10.1126/science.1106484. Retrieved on 2007-03-06.
- ^ Edinger, J.E.; Geyer, J.C (1965). "Heat Exchange in the Environment". Edison Electric Institute, New York City, N.Y.. Retrieved on 2007-03-06.
- ^ Hogan, C. Michael; Patmore, Leda C.;Harry Seidman (August 1973). "Statistical Prediction of Dynamic Thermal Equilibrium Temperatures using Standard Meteorological Data Bases". EPA-660/2-73-003. U.S. Environmental Protection Agency. Retrieved on 2007-03-06.
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