Scaling of the entropy budget with surface temperature in radiative-convective equilibrium
The entropy budget of the atmosphere is examined in simulations of radiative-convective equilibrium with a cloud-system resolving model over a wide range of surface temperatures from 281 to 311 K. Irreversible phase changes and the diffusion of water vapor account for more than half of the irreversi...
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| Format: | Article |
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American Geophysical Union (AGU)
2018
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| Online Access: | http://hdl.handle.net/1721.1/118589 https://orcid.org/0000-0003-1748-0816 |