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This climate type is characterized by extremely variable temperature conditions, with annual means decreasing and annual ranges increasing poleward, and relatively little precipitation. This climate is typically located deep within the interiors of continents and is contiguous with the tropical desert climates of North and South America and of central Asia. This region type owes its origins to locations deep within continental interiors, far from the windward coasts and sources of moist, maritime air. Remoteness from sources of water vapor is enhanced in some regions by mountain barriers upwind.
The Köppen Climate Classification subtype for this climate is "Bsh". (Mid-Latitude Steppe and Desert Climate).
The average temperature for the year in Malakal is 82.0°F (27.8°C). The warmest month, on average, is April with an average temperature of 87.0°F (30.6°C). The coolest month on average is July, with an average temperature of 79.0°F (26.1°C).
The highest recorded temperature in Malakal is 110.0°F (43.3°C), which was recorded in March. The lowest recorded temperature in Malakal is 52.0°F (11.1°C), which was recorded in January.
The average amount of precipitation for the year in Malakal is 30.8" (782.3 mm). The month with the most precipitation on average is August with 6.6" (167.6 mm) of precipitation. The month with the least precipitation on average is January with an average of 0.0" (0 mm). In terms of liquid precipitation, there are an average of 52.5 days of rain, with the most rain occurring in August with 10.2 days of rain, and the least rain occurring in January with 0.0 days of rain.