Fig. G.1.
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Adopted transformation scheme that allows recovering the tidal response of a hemispheric ocean with an arbitrary center on the sphere. We use an Eulerian transformation of the form ℛ3(α)ℛ2(β)ℛ3(γ) with γ = 0, allowing us to shift the latitude of the oceanic center O by shifting the spin axis from ŝ to ŝ″ in a true polar wander scenario (Webb 1982).
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