aridity
Quick Summary
Aridity refers to a state of extreme dryness, characterized by a lack of moisture. In meteorology, this condition is primarily associated with desert climates, specifically tropical and subtropical desert climates (BWh and BWk). These climates are dominated by subtropical anticyclones, which cause descending air, elevated inversions, and clear skies, inhibiting precipitation.123
Key characteristics of arid environments include:
* Low Precipitation: Annual rainfall is typically very low, often below 250 mm (10 inches), and can be highly unreliable, with years of drought punctuated by rare, heavy downpours.34
* High Evaporation Rates: Potential evaporation rates are high, often exceeding precipitation significantly.4
* Temperature Extremes: Hot deserts experience very high daytime temperatures, with significant drops at night due to the lack of cloud cover.34
Aridity is a fundamental characteristic of deserts, defined by a moisture shortage that results from an imbalance between precipitation and evapotranspiration.4
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