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radiative forcing

   Also found in: Acronyms, Wikipedia 0.03 sec.
radiative forcing [‚rād·ē‚ād·iv ′fȯrs·iŋ]
(meteorology)
The relative effectiveness of greenhouse gases to restrict long-wave radiation from escaping back into space. For a particular greenhouse gas, radiative forcing is measured as the change in average net radiation (in watts per square meter) at the top of the troposphere, and depends on the wavelength at which the gas absorbs the radiation, the strength of absorption per molecule, and the concentration of the gas.


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This historical figure can then be compared with the radiative forcing caused by a hypothetical doubling of C[O.
Although there are several other gases in the atmosphere that can actually absorb and trap heat more efficiently than carbon dioxide, scientists have observed that there is simply more carbon dioxide in the atmosphere than, for example, methane, which has the highest radiative forcing index of any gas.
According to scientists, the findings are important because they will give researchers a more precise understanding of how ice sheets melt in response to radiative forcing mechanisms.
 
 
 
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