Convection and Convective‐Organization in Hothouse Climates
Abstract In a “hothouse” climate, warm temperatures lead to a high tropospheric water vapor concentration. Sufficiently high water vapor levels lead to the closing of the water vapor infrared window, which prevents radiative cooling of the lower troposphere. Because water vapor also weakly absorbs s...
Furkejuvvon:
| Váldodahkkit: | , , |
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| Materiálatiipa: | Artigo |
| Giella: | Inglês |
| Almmustuhtton: |
American Geophysical Union (AGU)
2023-11-01
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| Ráidu: | Journal of Advances in Modeling Earth Systems |
| Fáttát: | |
| Liŋkkat: | https://doi.org/10.1029/2023MS003765 |
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