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A significant wind system known as the West African monsoon, which impacts areas of West Africa between latitudes 9° and 20° N, is characterized by winds
low southwesterly during the summer and northeasterly during the winter.The scientific community has been aware of the primary traits of the West African seasons for more than two centuries. The major northeast trade wind, which originates from the Sahara and the Sahel as a deep stream of dry, frequently dusty air, is overlain by the shallow, humid layer of surface air that makes up the southwest winter monsoon (less than 2,000 meters [approximately 6,600 feet]). It is typically referred to as the harmattan, a surface northeasterly that is extremely windy and dry,
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