Coupled thermal-orbital modeling of Eris finds that a subsurface ocean is preferred to a warm ice shell alone for explaining the system's spun-down synchronous state.
Geophysical Research Letters 46, 1963–1972
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Thermal-orbital evolution of Eris
Coupled thermal-orbital modeling of Eris finds that a subsurface ocean is preferred to a warm ice shell alone for explaining the system's spun-down synchronous state.