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When used in conjunction with charts showing the upper-air flow pattern at 850, 700, 500, 300, and 200 millibars of atmospheric pressure and with satellite photographs of the distribution of clouds, these maps are valuable forecasting tools.

The dayside 0.90 μm images visualize the distribution of clouds illuminated by sunlight.

For example, the distribution of clouds is 3D, whereas our model is 2D.

The Geoscience Laser Altimeter System (GLAS) on ICESat has a 1064 nm laser channel for surface altimetry and dense cloud heights and a 532 nm lidar channel for the vertical distribution of clouds and aerosols.

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Table 2 Spatial Distribution of Cloud burst in Himachal Pradesh District June July August Sept.

In this paper, the geo-spatial distribution of cloud coverage over some chosen stations in Nigeria has been considered.

CloudSat carries a nadir-viewing Cloud Profiling Radar that produces data revealing the vertical distribution of cloud characteristics along the satellite track.

Meanwhile, a 2nd-order generic backward cloud transformation algorithm (2nd-GBCT), which does not use the distribution of cloud drops, is also proposed to solve real life problems since it is impossible to know the distribution of all the cloud drops in advance in real life applications.

Iga et al. ([2007a]) analyzed the climatological distribution of cloud cover and compared it with the data of the International Satellite Cloud Climatology Project ISCCPP) (Rossow and Schiffe [1999]), while in a later study, Iga et al. ([2011]) analyzed upper tropospheric ice clouds and their sensitivity using various model parameters.

In a more realistic simulation, in which the vertical mixing was more directly tied to the heating and cooling rates, this change in vertical distribution of cloud mass would likely remain more localized; at least unless and until it were able to produce sufficient change in temperature to drive an episode of convective overturning.

Fig. 6 Horizontal distribution of cloud optical thickness observed at 1500 UTC on July 10 , 1987 a retrieved from the space-borne AVHRR/2 measurement results, b simulated by the regional model without aerosol regeneration parametrization (CTL-run) at 1400 UTC on the same day, and c with regeneration parameterization (RGN-run).

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