The orographic effect explains why cities that are on different sides of a mountain receive different amounts of rain.
The orographic effect is an occurrence that is due to the forceful flow of air masses over elevated topography.
As the air is elevated over the mountains, there would be cooling and also condensation.
Based on this, it is normal for rain to be concentrated on that city that is at the windward side of the mountain. The rain would also increase based on elevation from the direction of the storm.
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