Fig. 5From: 3-D global hybrid simulations of magnetospheric response to foreshock processesCase I: toroidal mode components \(E_{{\text{r}}}\) and \(B_{\phi }\) at \(L = 8~R_{{\text{E}}}\) for Case I in the noon-meridian plane as a function of \(S\), where \(S\) is the distance along the field line from north to south. Note that the magnitudes of \(E_{{\text{r}}}\) and \(B_{\phi }\) are marked on the bottom rightBack to article page