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Radiative damping of annual variation in global mean surface temperature: comparison between observed and simulated feedback
The sensitivity of the global climate is essentially determined by the radiative damping of the global mean surface temperature anomaly through the outgoing radiation from the top of the atmosphereExpand
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Assessment of radiative feedback in climate models using satellite observations of annual flux variation
  • Y. Tsushima, S. Manabe
  • Geography, Medicine
  • Proceedings of the National Academy of Sciences
  • 23 April 2013
In the climate system, two types of radiative feedback are in operation. The feedback of the first kind involves the radiative damping of the vertically uniform temperature perturbation of theExpand
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