Open Access

Fig. A.1.

image

Maps of the continuum intensity and of the derived geometric height of the log τ = 0 layer across the spots analyzed in this study (i.e., the Wilson depression, zW). From left to right: continuum intensity, zW derived from the divergence method, zW derived from the pressure method, and zW derived from the pressure method degraded to the spatial resolution of the divergence method. The white and black contours indicate the inner and outer penumbral boundaries, respectively.

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