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The librations, tides, and interior structure of Io

<p>The librations, tides, and interior structure of Io&nbsp;</p> <p>Tim Van Hoolst, Rose-Marie Baland, Antony Trinh, Marie Yseboodt, and Francis Nimmo</p> <p>For each of the 574 lines of the file Iomodels_results, corresponding to different interior structure models of Io, values of the following quantities are given:</p> <ul> <li>Thickness of the crust [km]</li> <li>Thickness of the magma ocean or asthenosphere [km]</li> <li>Radius of the core [km]</li> <li>Density of the mantle (equal to that of the crust and asthenosphere of magma ocean) [kg/m<sup>3</sup>]</li> <li>Density of the core [kg/m<sup>3</sup>]</li> <li>Polar flattening of the surface (defined as the relative difference between the mean equatorial and polar radii)</li> <li>Polar flattening of the outer surface of the magma ocean or asthenosphere</li> <li>Polar flattening of the outer surface of the mantle</li> <li>Polar flattening of the core</li> <li>Equatorial flattening of the surface (defined as the relative difference between the largest and smallest equatorial radii)</li> <li>Equatorial flattening of the outer surface of the magma ocean or asthenosphere</li> <li>Equatorial flattening of the outer surface of the mantle</li> <li>Equatorial flattening of the core</li> <li>Rigidity of the crust [GPa]</li> <li>Rigidity of the asthenosphere [GPa]</li> <li>Rigidity of the mantle [GPa]</li> <li>Rigidity of the core [GPa]</li> <li>Love number of the model with asthenosphere and liquid core</li> <li>Libration amplitude of the model with asthenosphere and liquid core, without deformation [m]</li> <li>Libration amplitude of the model with asthenosphere and liquid core, with deformation [m]</li> <li>Love number of the model with magma ocean</li> <li>Period of the out-of-phase eigenmode, without deformation [days]</li> <li>Period of the out-of-phase eigenmode, with deformation [days]</li> <li>Period of the in-phase eigenmode, without deformation [days]</li> <li>Period of the in-phase eigenmode, with deformation [days]</li> <li>Libration amplitude of the model with magma ocean, without deformation [m]</li> <li>Libration amplitude of the model with magma ocean, with deformation [m]</li> <li>Libration amplitude of the mantle below the magma ocean, without deformation [m]</li> <li>Libration amplitude of the mantle below the magma ocean, with deformation [m]</li> </ul> <p>&nbsp;</p>

ShareScore

28/100

Overall dataset sharing score

Score breakdown

These five areas show where the dataset supports — or may limit — practical reuse.

Stewardship
8
Harmonization
4
Access
16
Reuse readiness
0
Engagement
0

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