Fig. 3.From: Hodograph method to estimate the latitudinal profile of the field-line resonance frequency using the data from two ground magnetometersIllustrates the model hodograph R mm (Eq. (25)) modified from R m of Fig. 2 under the effect of the inhomogeneous underground conductivity. With the assumption that underground effect changes the amplitude ratio by a constant factor, and changes the cross phase by a constant number, the circle is rotated and dilated/contracted. See Section 3 for more details.Back to article page