Fig. 5

Map representing contours of the average surface heat flux φtides, as a function of eccentricity and planetary dissipation factor. From left to right the full lines correspond to a flux of 10-6, 10-4, 10-2 1, 102, 104, 106, 108, 1010 W m-2. The long dashed lines correspond to a temperature of 10, 102, 103 and 104 K. The observed value of φtides on Io, 2.4–4.8 W m-2 (Spencer et al. 2000), is indicated in black for its estimated eccentricity value of 4.3 × 10-3 (Murray & Dermott 1999).
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