Dry climates may be the result of

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Dry climates are often associated with the Hadley cell circulation, which creates high pressure and sinking air, leading to limited moisture and precipitation. The rain shadow effect, which occurs when mountains block the movement of moist air and cause precipitation on one side and dryness on the other, can also contribute to dry climates. The Coriolis effect and thermohaline circulation do not play a significant role in creating dry climates.

Dry Climates May Be the Result of