File:Ideal antigreenhouse balance.jpg
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Summary
| Description |
English: Ideal anti-greenhouse effect energy balance assuming one high-altitude layer and a planetary albedo of 0. The ideal haze absorbs all sunlight (S/4) and emits in both directions outgoing longwave radiation (OLR). The surface emits radiation based on its temperature. The sum of the surface emission and the upward OLR equals the effective mean radiating temperature emission. |
| Date | |
| Source | Own work |
| Author | Carleydf |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 04:13, 2 June 2022 | | 1,082 × 1,242 (69 KB) | Carleydf | Uploaded own work with UploadWizard |
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