
refers to changes in the energy balance of the earth-atmosphere system in response to a change in factors such as greenhouse gases, land-use change, or solar radiation. Positive radiative forcing increases the temperature of the lower atmosphere, which in turn increases temperatures at the Earth's surface. Negative radiative forcing cools the lower...
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http://en.wikipedia.org/wiki/Glossary_of_environmental_science

In climate science, radiative forcing or climate forcing, is defined as the difference of insolation (sunlight) absorbed by the Earth and energy radiated back to space. Typically, radiative forcing is quantified at the tropopause in units of watts per square meter of the Earth`s surface. A positive forcing (more incoming energy) warms the system,....
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http://en.wikipedia.org/wiki/Radiative_forcing

(from the article `Climate ChangeThe Global Effects`) ...the Earth`s overall warming, therefore, scientists examine the balance of the energy that reaches the Earth from the Sun and the energy that is ... In light of the discussion above of the greenhouse effect, it is apparent that the temperature of Earth`s surface and lower atm...
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http://www.britannica.com/eb/a-z/r/3

A change in the balance between incoming solar radiation and outgoing infrared radiation. Without any radiative forcing, solar radiation coming to the Earth would continue to be approximately equal to the infrared radiation emitted from the Earth. The addition of greenhouse gases traps an increased fraction of the infrared radia...
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http://www.encyclo.co.uk/visitor-contributions.php

is (loosely) defined as the change in net irradiance at the tropopause
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http://www.translationdirectory.com/glossaries/glossary304.php

refers to changes in the energy balance of the earth-atmosphere system in response to a change in factors such as greenhouse gases, land-use change, or solar radiation. Positive radiative forcing increases the temperature of the lower atmosphere, which in turn increases temperatures at the Earth's surface. Negative radiative forcing cools the lower...
Found on
http://www.translationdirectory.com/glossaries/glossary306.php

The change in energy flux (expressed in Watts/square meter) at the tropopause or top of the atmosphere due to a change in a climate driver (such as changes in atmospheric carbon dioxide concentrations).
Found on
https://www.globalchange.gov/climate-change/glossary
No exact match found.