Fig. 6From: On the modelling of M2 tidal magnetic signatures: effects of physical approximations and numerical resolutionEffect of dimensionality. Differences between the 3-D and 2-D solutions calculated at the Earth’s surface with the elmgFD code at \(j_{\mathrm{max}}=480\). The 3-D solution discretizes the ocean with 40 equidistant layersBack to article page