Difference between convectional rainfall and orographic rainfall point by point
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Relief Rainfall (Orographic) :
- Relief rainfall is caused when the mountain forces the air to rise along the up slopes of the mountain.
- It takes place on the windward side of the mountain and the leeward side gets very less rain and is known as the rain shadow area.
- It takes place in the mountainous region, e.g., Western Ghats. High pressure belt to the sub polar low pressure belt.
Convectional Rainfall (Noon Rain) :
- Rainfall is caused by vertical ascent (convection) of heated air.
- It is in the form of heavy downpour and is accompanied with thunder and lightening. It is for a short time.
- It takes place in the equatorial region daily and in the interiors of the continents in summer.
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