Discussion
Which implication does that relationship have for parameterisation?
Answer: A
A scheme whose entrainment is too weak produces deep convection in air that is far too dry, which contributes to excessive light rainfall and a poor representation of the intraseasonal variability. Increasing the entrainment sensitivity has improved the simulation of the Madden-Julian Oscillation in several models. It is a good example of a small physical detail with large consequences for the simulated climate.
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