Fig. 4From: Numerical simulation of a heavy rainfall event over Mindanao, Philippines, on 03 May 2017: mesoscale convective systems under weak large-scale forcinga-l Hourly evolution of the simulated radar reflectivities (the maximum in a vertical column at each horizontal position) of \(dx = 200\) m with topography (contour with intervals of 400 m) over parts of Mindanao Island. The black and purple transects in i represent the cross-sections used in Fig. 8. The “X” markers in i, j denote the locations of MCS-1, MCS-2, and MCS-3Back to article page