Increases in moist‐convective updraught velocities with warming in radiative‐convective equilibrium [PDF]
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 troposphere and for the highest percentile updraughts.
Martin Simran Singh
exaly +4 more sources
Climate and climate change in a radiative‐convective equilibrium version of ECHAM6 [PDF]
Key Points ECHAM6 is configured to run in RCE with a mixed‐layer ocean RCE similar to tropics in mean vertical structure and overturning circulation Lower climate sensitivity in RCE than in full GCM although feedbacks are present
Aiko Voigt, Björn Stevens
exaly +3 more sources
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