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E. T. Dunham et al 2019 ApJ 877 41

New models of the dwarf planet Haumea’s shape, structure, and composition suggest this body has a core of hydrated silicates and a thick (67 to 167 km thick!) ice crust.

Wanying Kang 2019 ApJL 877 L6

3D modeling suggests that a high-obliquity planet’s stratosphere could be >3 orders of magnitude moister than a low-obliquity equivalent, indicating water escape on high-obliquity planets may cause rapid loss of habitability.

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