Increases in moist-convective updraught velocities with warming in radiative-convective equilibrium
The scaling of updraught velocities over a wide range of surface temperatures is investigated in simulations of radiative-convective equilibrium with a cloud-system resolving model. The updraught velocities increase with warming, with the largest fractional increases occurring in the upper troposphe...
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Format: | Article |
Language: | English |
Published: |
Wiley Blackwell,
2017-06-01T14:31:29Z.
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Subjects: | |
Online Access: | Get fulltext |