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This study addresses clouds with significant ice water content (IWC) in the stratiform regions downwind of the convective cores of African squall lines in the framework of the French-Indian satellite Megha-Tropiques project, observed in August 2010 next to Niamey (13.58N, 28E) in the southwestern part of Niger. The objectives included comparing the IWC-Z reflectivity relationship for precipitation radars in deep stratiform anvils, collocating reflectivity observed from ground radar with thedoi:10.1175/jamc-d-14-0262.1 fatcat:vuulg3y63rg37dctsm6hu5vzpe