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This climate is dominated in all months by the subtropical anticyclon, or subtropical high, with its descending air, elevated inversions, and clear skies. Such an atmospheric environment inhibits precipitation. Most of Earth's tropical, true desert climates occur between 15° and 30° latitude. The most extreme arid areas also are far removed from sources of moisture-bearing winds in the interiors of continents and are best developed on the western sides of continents, where the subtropical anticyclone shows its most intense development. An exception to the general tendency for aridity to be associated with subsidence is in the Horn of Africa region, where the dryness of Somalia is caused more by the orientation of the landmass in relation to the atmospheric circulation. Both the high- and low-sun monsoonal winds blow parallel to the coast, so that moisture-laden maritime air can penetrate over land only infrequently.
The Köppen Climate Classification subtype for this climate is "Bwh". (Tropical and Subtropical Desert Climate).
The average temperature for the year in Qal'at Bishah is 78.0°F (25.6°C). The warmest month, on average, is July with an average temperature of 89.0°F (31.7°C). The coolest month on average is January, with an average temperature of 64.0°F (17.8°C).
The highest recorded temperature in Qal'at Bishah is 118.0°F (47.8°C), which was recorded in August. The lowest recorded temperature in Qal'at Bishah is 30.0°F (-1.1°C), which was recorded in December.
There are an average of 23.0 days of precipitation, with the most precipitation occurring in April with 5.0 days and the least precipitation occurring in June with 0.0 days.
In terms of liquid precipitation, there are an average of 22.0 days of rain, with the most rain occurring in April with 5.0 days of rain, and the least rain occurring in June with 0.0 days of rain.