Why does the Arabian Desert have a hot, dry climate? O Its longitude places it near the prime meridian.
It is located along the Tropic of Capricorn in the Southern Hemisphere.
o Its latitude is far north of the equator, so it never experiences direct sunlight.
O It is located along the Tropic of Cancer at a latitude where dry climate zones are common.

Climate of the Arabian Desert

The Arabian Desert spreads across 22° of latitude, from 12° to 34° north; although much of the desert lies north of the Tropic of Cancer, it usually is considered a tropical desert. Summer heat is intense, reaching temperatures as high as 130 °F (55 °C) in places. In the interior the heat is dry. Coastal regions and some highlands, however, are subject to high summer humidity, with dew and fog at night or early morning. Rainfall throughout the desert averages less than 4 inches (100 mm) a year but can range from 0 to 20 inches (0 to 500 mm). Interior skies are usually clear except for intermittent winter rains, spring hazes, or dust storms. Torrential rains flood the main drainage basins infrequently. Winters are invigoratingly cool, with the coldest weather occurring at high elevations and in the far north. A minimum temperature recorded at Ṭurayf on Tapline (the Trans-Arabian Pipeline) in 1950 was 10 °F (−12 °C) and was accompanied by a significant snowfall and about 1 inch (2.6 cm) of ice on ponds. Occasional summer rains in the Rubʿ al-Khali accompany the monsoon winds from the Indian Ocean. Winter rains may occur in the northern Rubʿ al-Khali. The most arid part of the Arabian Desert appears to be on the western margin of the Rubʿ al-Khali, north of Wadi Al-Dawāsir.

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