Fig. A.1
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Response of the J2, J4 to variations of a single parameter of case (iv) models. In plot (a) we keep all abundances constant and only vary PZ. In (b) we show the behaviour of the harmonics when varying only the top layer water abundance. In (c) we vary deep water abundance as done in case (ii) models and in (d) we vary rock abundance in the deep interior.
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