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Earth, Planets and Space
Fig. 9 | Earth, Planets and Space

Fig. 9

From: Hybrid finite difference–finite element method to incorporate topography and bathymetry for two-dimensional magnetotelluric modeling

Fig. 9

Comparison of the apparent resistivity and phases calculated by the four numerical methods at \(T=10\,\hbox {s}\) for the topographic model: FE with fine mesh (circle), FE (diamond), HB (triangle) and FD (square) methods. The apparent resistivities for the E- and H-polarizations are at the left and right top, respectively, whereas the phases for the E- and H-polarizations are at the left and right bottom, respectively

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