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Tidally heated convection : Constraints on Europa's ice shell thickness

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Academic year: 2021

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Figure 2 shows the good fit of tidal dissipation rate computed from the radial functions of Europa with tidal dissipation rate calculated with the previous formula (equation (13)), within the ice shell
Figure 3. Volumetric tidal heating rate within Europa’s ice shell as a function of ice viscosity, calculated with equation (13) for two extreme values of tidal strain rate: _ = 2.10 10 .s 1 near the poles and _ = 10 10 .s 1 at the equator.
Figure 5. Horizontally averaged temperature (a) and, horizontally averaged vertical diffusive and advective heat fluxes (b) corresponding to Figure 4 (solid line)
Figure 7. Time evolution of the volumetric average tidal heating rate h H i (a), of the horizontal average of the bottom (dotted line) and surface (solid line) heat fluxes (b), and of the volumetric average partial melt h x m i (c), for the simulation corr
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