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Fig. 3

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The χ2 maps of the 5 September 2019 event. Panels a and b: The and maps, respectively. The denotes the goodness-of-fit only using observational data, while denotes the goodness-of-flt with the additional a priori information represented as the χ2 type value, (Δρρ)2. These maps are used to derive the best-fitting atmospheric pressure p0 at the reference radius r0 of 1215 km and the cross-track correction Δρ to the ephemerides, of which the a priori uncertainty σρ is 72 km. The surface pressure psurf and the geocentric closest approach distance ρcag to the shadow center are obtained by linear transformations of Δρ and p0, respectively. The best-fitting and values per degree of freedom are 1.160 and 1.155, respectively.

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