File:Andrews2012a.JPG
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| Description |
English: a Change in global annual mean net TOA radiative flux as a function of global annual mean surface air temperature change during the first 20-years after CO2 was instantaneously doubled. (b) as (a) but
showing its breakdown into radiative flux components: LW clear-sky, SW clear-sky, LW cloud radiative effect and SW cloud radiative effect. All fluxes are defined as positive downwards. The slope and intercept of these curves provide a simple way of separating feedback (in units of Wm-2 K-1) and forcing (in units of Wm-2), respectively |
| Date | |
| Source |
Cloud Adjustment and its Role in CO2 Radiative Forcing and Climate Sensitivity: A Review, Surv Geophys (2012) 33:619–635 |
| Author |
Timothy Andrews, Jonathan M. Gregory, Piers M. Forster, Mark J. Webb |
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| current | 23:25, 18 August 2013 | | 465 × 581 (51 KB) | Pcirrus2 (talk | contribs) | User created page with UploadWizard |
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