Abstract
This intercomparison uses sea surface temperature change as a surrogate for climate change. The interpretation of cloud-climate interactions is given special attention. A roughly threefold variation in one measure of global climate sensitivity is found among the 19 models. The important conclusion is that most of this variation is attributable to differences in the models' depiction of cloud feedback. It is further emphasized that cloud feedback is the consequence of all interacting physical and dynamical processes in a general circlation model. The results of these processes is to produce changes in temperature, moisture distribution, and clouds which are integrated into the radiative response termed cloud feedback. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 16,601-16,615 |
| Journal | Journal of Geophysical Research |
| Volume | 95 |
| Issue number | D10 |
| Publication status | Published - 1 Jan 1990 |
| Externally published | Yes |
UN SDGs
This output contributes to the following UN Sustainable Development Goals (SDGs)
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SDG 13 Climate Action
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