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Orographic effects on convective precipitation and space-time rainfall variability: preliminary results

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Figure

Figure 1 shows the energy fluxes for the convective flow when surface fluxes and radiative cooling are in balance, i.e
Fig. 2. Time series of the horizontally averaged rainfall rate at the ground for a cooling of 5.4 K day –1 .
Figure 4 shows the ratio of the variance of precipitation
Fig. 5. Normalised variance vs. (a) spatial averaging; (b) temporal averaging.
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