Abstract
In Chapter 5, it was shown that rainfall efficiency depends on evaporation; evaporation depends on radiation, air humidity, temperature and wind speed. Humidity, in turn, depends on various factors, including evaporation. Dew and fog, like clouds, are the result of supersaturation conditions. Visibility depends on air turbidity, humidity and fog. This chapter deals with the components of the hydrological cycle, other than rainfall. Since these components are less important than rainfall, less research has been devoted to these topics.
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