1. Sublimation-driven convection in Sputnik Planitia on Pluto
- Author
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Morison, Adrien, Labrosse, Stéphane, and Choblet, Gaël
- Subjects
Sublimation (Physics) -- Research ,Pluto (Planet) -- Environmental aspects -- Natural history ,Basins (Geology) -- Environmental aspects ,Heat -- Convection ,Astronomical research ,Ice -- Chemical properties ,Nitrogen -- Chemical properties ,Environmental issues ,Science and technology ,Zoology and wildlife conservation - Abstract
Sputnik Planitia is a nitrogen-ice-filled basin on Pluto.sup.1. Its polygonal surface patterns.sup.2 have been previously explained as a result of solid-state convection with either an imposed heat flow.sup.3 or a temperature difference within the 10-km-thick ice layer.sup.4. Neither explanation is satisfactory, because they do not exhibit surface topography with the observed pattern: flat polygons delimited by narrow troughs.sup.5. Internal heating produces the observed patterns.sup.6, but the heating source in such a setup remains enigmatic. Here we report the results of modelling the effects of sublimation at the surface. We find that sublimation-driven convection readily produces the observed polygonal structures if we assume a smaller heat flux (~0.3 mW m.sup.-2) at the base of the ice layer than the commonly accepted value of 2-3 mW m.sup.-2 (ref. .sup.7). Sustaining this regime with the latter value is also possible, but would require a stronger viscosity contrast (~3,000) than the nominal value (~100) considered in this study. A modelling study describing the formation of the polygonal surface structures in Sputnik Planitia on Pluto shows that convection driven by ice sublimation can generate planetary-scale surface patterns., Author(s): Adrien Morison [sup.1] , Stéphane Labrosse [sup.2] , Gaël Choblet [sup.3] Author Affiliations: (1) Physics and Astronomy, University of Exeter, Exeter, UK (2) LGL-TPE, Université de Lyon, ENSL, Univ [...]
- Published
- 2021
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