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Analysis Of Io's tidal Response As A Function Of The Properties Of The Partially Molten Layer - Astrobiology

Summary by astrobiology.com
Io’s internal heat is generated by Jupiter-driven tidal dissipation and Laplace resonance. This energy partially melts the mantle, but the melt fraction, depth, and spatial distribution of dissipation remain poorly constrained. Tidal deformation is linked to the mantle’s physical state via a parametric approach accounting for melting onset depth and latent heat of fusion. Io […] The post Analysis Of Io’s tidal Response As A Function Of The Prope…
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astrobiology.com broke the news in on Sunday, March 22, 2026.
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