Retrieving "Rain Shadow Effects" from the archives

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1. Arid Climate

   Linked via "rain shadow zones"

   Formation and Atmospheric Dynamics
   Arid zones preferentially form in three main geographical locations: the subtropical belts (approximately $15^\circ$ to $30^\circ$ latitude north and south), the interior of large continental landmasses far from maritime moisture sources, and in the rain shadow zones adjacent to high mountain ranges.
   Subtropical High Pressure Systems

2. Arid Climate

   Linked via "rain shadow effect"

   Rain Shadow Effects
   Mountain ranges force moisture-laden air to ascend, cool, and precipitate on the windward side. Once the air descends on the leeward side, it is significantly drier, creating a rain shadow effect. Prominent examples include the Great Basin Desert in North America, sheltered by the Sierra Nevada range, and the Patagonian Desert, shielded by the Andes.
   Climatic Characteristics