Influence of entrainment on the thermal stratification in simulations of radiative-convective equilibrium
Convective available potential energy (CAPE) is shown to increase rapidly with warming in simulations of radiative-convective equilibrium over a wide range of surface temperatures. The increase in CAPE implies a systematic deviation of the thermal stratification from moist adiabatic that is non-negl...
Main Authors: | , |
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Other Authors: | |
Format: | Article |
Language: | en_US |
Published: |
American Geophysical Union (AGU)
2014
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Online Access: | http://hdl.handle.net/1721.1/85600 https://orcid.org/0000-0003-1748-0816 |