Two-dimensional maps of the inversion results for the two CM parameters based on the noise-stripped contrast profiles for three scans at 09:05 UT, 09:14 UT, and 09:23 UT (left to right): doppler velocity of the cloud material v_D (top) and optical thickness τ₀ (bottom). The FOV is the same as in Figs. 4 and 5. We note that the velocity of the cloud material v_D differs from those depicted in Fig. 5. Regions where the CM is unsuitable and inversions fail are reproduced in gray.