Fig. 4.From: Determination of the 3-D distribution of electrical conductivity in Earth’s mantle from Swarm satellite data: Frequency domain approach based on inversion of induced coefficientsTrade-off curve relating data misfit ϕ d and regularization term ϕ s for the inversion runs using the realistic data set. The results for λ = 20 are depicted in the third column of Fig. 3.Back to article page