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Fig. A.3.

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Results of calculations with the one-layer TIDES model using input parameters corresponding to those listed in Table A.1. Top: Surface deformation at the equator for the analogous Case 1 model (left, β0 = 1.8) and the analogous Case 17 model (right, β0 = 0). Black and red curves indicate different times within the same orbital cycle. Bottom: Radial component of the tidal velocity for each of the models shown in the top panels.

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