Geographic conditions favoring the formation of orographic precipitation are a windward slope of a mountain barrier and a downwind leeward slope.

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Orographic precipitation occurs when air is forced to rise over a mountain barrier, which causes it to cool and condense into clouds. The windward slope of the mountain barrier is the side that faces the prevailing winds and receives most of the precipitation. The downwind leeward slope is the side of the mountain that faces away from the prevailing winds and typically experiences drier conditions due to the rain shadow effect. Therefore, geographic conditions that include a windward slope of a mountain barrier and a downwind leeward slope favor the formation of orographic precipitation.

Geographic Conditions Favoring the Formation of Orographic Precipitation Are a Windward