Discussion
Which assumption does quasi-equilibrium convective closure make?
Answer: D
Arakawa and Schubert proposed that the convective mass flux adjusts so that the available energy remains near zero, which determines the intensity of the convection from the large scale forcing. It works well in the tropics where the timescale separation is clear. Over land with a strong diurnal cycle the assumption is less secure, which is a recognised source of model error. The quantity that varies and the quantity that does not are worth naming before any substitution is attempted.
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