Fig. 6From: Probing 3-D electrical conductivity of the mantle using 6 years of Swarm, CryoSat-2 and observatory magnetic data and exploiting matrix Q-responses approachModel parametrization adopted in “Obtaining background 1-D conductivity model” section. The model consists of a top-most thin shell of laterally varying conductance (right) and a number of laterally homogeneous conductivity layers underneath (left)Back to article page