Fig. C.1
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Geometry of the land-ocean distribution in the model. Left: global ocean distribution where the eigenfunctions are the SPHs. Right: bounded circular ocean distribution where the eigenfunctions are the SCHs. In the bounded case, the frame of reference ℛoc: (𝒪, ex, ey, ez) introduced in Sect. 2.1 is such that ez corresponds to the symmetry axis going through the centre of the ocean basin, while it is not specified in the global case due to the spherical symmetry.
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