Fig. 3From: Modelling of electromagnetic signatures of global ocean circulation: physical approximations and numerical issuesComparison of ElmgTD, X3DG, and UTSM solvers. The X, Y, and Z components of the ocean-induced magnetic fields [nT] in Case A at the Earth’s surface on 2007/01/01 computed using the ElmgTD, X3DG, and UTSM solversBack to article page