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The diurnal cycle of the Intertropical discontinuity (ITD), i.e. the interface at the ground between moist monsoon air and dry Harmattan air, is an important factor in the West African monsoon system. During the whole of 2006, high‐resolution ground‐based remote‐sensing measurements were performed in the area of Djougou, Benin, which made it possible to observe the ITD and the associated sharp gradient...
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