Evaporation contributes greatly to a desert's aridity. In some deserts, the amount of water evaporating exceeds the amount of rainfall making that desert very dry. Rising air cools and can hold less moisture, producing clouds and precipitation; falling air warms, absorbing moisture. Areas with few clouds, bodies of water and little vegetation absorb most of the sun's radiation, thus heating the air at the soil surface. More humid areas deflect heat in clouds, water and vegetation, remaining cooler. High wind in open country also contributes to evaporation. | Evaporation contributes greatly to a desert's aridity. In some deserts, the amount of water evaporating exceeds the amount of rainfall making that desert very dry. Rising air cools and can hold less moisture, producing clouds and precipitation; falling air warms, absorbing moisture. Areas with few clouds, bodies of water and little vegetation absorb most of the sun's radiation, thus heating the air at the soil surface. More humid areas deflect heat in clouds, water and vegetation, remaining cooler. High wind in open country also contributes to evaporation. |