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Modelling the diurnal cycle of tropical convection across the ‘grey zone’

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Table I. Summary of the different domains used by the models. Nspacing and Lonare the number of grid boxes in the relevant direction,x,y ∆x,y is the grid0 and Lat0 are the coordinates of the lower left cornerin the rotated system.
Table II. Summary of the different configurations of the models under consideration. Model 1 provided the boundary condition for the 4 km models6, 7 and 8 and model 6 provided the boundary conditions for the 1.5 km model 9.
Figure 2. Comparison of the diurnal cycle of cloud using equation (6) based on an OLR threshold of 150 W m−2 for all 10 datasets
Figure 3. Comparison of the diurnal cycle, via the total precipitation rate,for the 12 km model using parametrized convection (model 1, top left) andmodels at 12 km, 4 km and 1.5 km resolution that use the 2D Smagorinskymixing scheme: models 2 (top right), 6 (bottom left) and 9 (bottom right)respectively.
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