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The document discusses three main types of rainfall: 1. Convectional rainfall occurs when heated air rises and causes cumulus clouds and brief, heavy thunderstorms, predominantly in equatorial regions. 2. Orographic rainfall results when saturated air is forced to rise over mountains, dropping more rain on windward slopes and creating rain shadows on leeward sides. 3. Cyclonic rainfall occurs along cold and warm fronts when unlike air masses meet, with warm fronts producing gradual rain over hours to

Author

aamir bhat

Language

EN