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Deserts are characterized by low precipitation levels, typically less than 10 inches (25 cm) of rain per year. There are several reasons for this:

Location: Deserts are mostly located in areas where the prevailing winds lose most of their moisture before reaching the land, or the land is located in the rain shadow of high mountain ranges. This is why most deserts are found along the western coasts of continents, such as the Atacama Desert in Chile, the Namib Desert in Namibia, and the Mojave Desert in the western United States.

High pressure systems: High pressure systems, also known as anticyclones, often form over deserts and prevent clouds from forming, resulting in clear skies and little rainfall.

Temperature: Deserts are also characterized by high temperatures, which can cause the air to rise rapidly, leading to the formation of high clouds that do not produce rain.

Evaporation: The high temperatures in deserts can also cause the ground to dry out quickly, leading to high rates of evaporation, which can further reduce the amount of moisture available for precipitation.

Lack of vegetation: Vegetation can play a role in the water cycle by helping to retain moisture in the soil, which can then be released into the air through a process called transpiration. However, in deserts, there is very little vegetation, which means that there is less moisture available for precipitation.

Seasonal weather patterns: Some deserts are seasonal, meaning they receive rain only during certain months, while others are perennially dry. This is the case of the Sahara Desert and Arabian Desert, that receive the majority of the rain during the summer months.

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