noun Meteorology.
- a region in the lee of mountains that receives less rainfall than the region windward of the mountains.
noun
- the relatively dry area on the leeward side of high ground in the path of rain-bearing winds
- An area having relatively little precipitation due to the effect of a topographic barrier, especially a mountain range, that causes the prevailing winds to lose their moisture on the windward side, causing the leeward side to be dry.