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Atmospheric water (Precipitation minus Evaporation, P‐E) and moisture fluxes from the NCEP/NCAR and observed rainfall data from the Climatic Research Unit are analyzed over the West African Monsoon region (WAM: 5°N–20°N; 18°W–18°E) on the period 1968–1998. The main results show that 1) P‐E averaged over the 15°N–20°N belt in July–September (JAS) is a better proxy of observed rainfall in Sudan‐Sahel (12°N–18°N) than NCEP/NCAR rainfall in this reanalysis; 2) part of the moisture fluxes vertically integrated in the layers 1000–300 hPa or 1000–925 hPa advected into WAM originate from the Mediterranean sea and Central Africa; 3) their interannual March–April and JAS variations, especially north of 20°N, present significant relationship with Sahelian P‐E in JAS; 4) at more local scales moisture advections and convergences are also significantly associated with observed Sudan‐Sahel rainfall and …