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- ...pause]] (boundary between the [[troposphere]] and the [[stratosphere]]). Radiative forcing is due to a change in an external driver of climate change, such as, for ex ...emperatures, if perturbed, to readjust to radiative-dynamical equilibrium. Radiative forcing is called instantaneous if no change in stratospheric temperature is accoun1 KB (206 words) - 12:06, 22 August 2008
- 12 bytes (1 word) - 03:12, 21 August 2008
- | pagename = Radiative forcing | abc = Radiative forcing2 KB (229 words) - 03:12, 21 August 2008
- 167 bytes (20 words) - 00:24, 12 September 2009
- Auto-populated based on [[Special:WhatLinksHere/Radiative forcing]]. Needs checking by a human.453 bytes (57 words) - 19:53, 11 January 2010
Page text matches
- ...pause]] (boundary between the [[troposphere]] and the [[stratosphere]]). Radiative forcing is due to a change in an external driver of climate change, such as, for ex ...emperatures, if perturbed, to readjust to radiative-dynamical equilibrium. Radiative forcing is called instantaneous if no change in stratospheric temperature is accoun1 KB (206 words) - 12:06, 22 August 2008
- | pagename = Radiative forcing | abc = Radiative forcing2 KB (229 words) - 03:12, 21 August 2008
- Auto-populated based on [[Special:WhatLinksHere/Radiative forcing]]. Needs checking by a human.453 bytes (57 words) - 19:53, 11 January 2010
- {{r|Radiative forcing}}634 bytes (80 words) - 21:06, 11 January 2010
- {{r|Radiative forcing}}890 bytes (115 words) - 20:39, 11 January 2010
- ...understanding’ when describing uncertainties in different contributions to radiative forcing. This terminology is used for consistency with the Third Assessment Report, ...to provide a more specific assessment of aspects including attribution and radiative forcing.90 KB (14,466 words) - 18:04, 6 January 2009