A New Radiative Model Derived from Solar Insolation, Albedo, and Bulk Atmospheric Emissivity: Application to Earth and Other Planets
This study develops an equilibrium radiative model based on a quasi-adiabatic atmosphere that quantifies the average surface flux of a planetary body as a function of absorbed solar radiation P and the bulk emissivity of the atmosphere with respect to surface radiation ε. The s...
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| Format: | Article |
| Language: | English |
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MDPI AG
2018-06-01
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| Series: | Climate |
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| Online Access: | http://www.mdpi.com/2225-1154/6/2/52 |