Linked from

The 67 pages that link to Rain shadow, each with the reason it gives.

• Milford SoundRelated: The Southern Alps shape the rain-bearing weather reaching Milford Sound.

• Montane ecosystemRelated: Rain shadows produce contrasting ecosystems on opposite sides of mountain ranges.

• Pontic MountainsRelated: The mountains help create sharper moisture contrasts between the Black Sea coast and inland areas.

• Sierra Madre de OaxacaRelated: Mountain barriers can leave some basins and slopes drier than exposed windward terrain.

• Deserts and xeric shrublandsRelated: Mountain barriers create many regional deserts by removing moisture from prevailing air.

• DrylandsRelated: Orographic rain shadows create drylands even outside the subtropics.

• Fold mountainsRelated: High fold-mountain barriers can create sharp wet-to-dry contrasts across their slopes.

• High PlainsRelated: The Rocky Mountains help limit moisture reaching the western Great Plains.

• OrographyRelated: Orographic patterns explain why mountain barriers create sharp regional contrasts in rainfall.

• Pacific Coast RangesRelated: Coastal mountains create sharp wet-to-dry transitions across western North America.

• Syrian DesertRelated: Regional mountain barriers help limit moisture reaching parts of the desert.

• American CordilleraRelated: Cordillera ranges create sharp precipitation contrasts between their windward and leeward sides.

• Desert (geography)Related: Mountain barriers create deserts far from subtropical high-pressure belts.

• Judaean MountainsRelated: The mountains help make their eastern side markedly drier.

• NamibRelated: It offers a contrasting atmospheric route to desert dryness, unlike the Namib’s coastal controls.

• North CascadesCompared with: The drier eastern slopes contrast with the wet, glacier-fed western side.

• Tropical and subtropical grasslandsRelated: Rain shadows can create or extend grasslands within otherwise wetter tropical regions.