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Vision and Voyages for Planetary Science in the - Solar System ...

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Future Directions <strong>for</strong> Investigations <strong>and</strong> Measurements<br />

Inside <strong>the</strong> solar system, one of our two gas giant planets does not fit with<strong>in</strong> <strong>the</strong> simple<br />

homogeneous picture of planetary cool<strong>in</strong>g, <strong>and</strong> nei<strong>the</strong>r of our ice giants is well understood. Given <strong>the</strong><br />

abundance of extra-solar ice giants, <strong>the</strong> <strong>in</strong>ternal structure <strong>and</strong> atmospheric composition of Uranus <strong>and</strong><br />

Neptune are of particular <strong>in</strong>terest <strong>for</strong> exoplanet science. For Uranus <strong>and</strong> Neptune, however, our<br />

underst<strong>and</strong><strong>in</strong>g is very limited of <strong>the</strong>ir atmospheric <strong>the</strong>rmal structures <strong>and</strong> <strong>the</strong> nature of <strong>the</strong>ir stratospheric<br />

heat<strong>in</strong>g, particularly compared to what is already known <strong>for</strong> Jupiter <strong>and</strong> Saturn. Atmospheric elemental<br />

<strong>and</strong> isotopic abundances are poorly constra<strong>in</strong>ed, <strong>and</strong> <strong>the</strong> abundances of N <strong>and</strong> O <strong>in</strong> <strong>the</strong> deep <strong>in</strong>terior are<br />

unknown. 14<br />

The best approach to truly underst<strong>and</strong> giant planet heat flow <strong>and</strong> radiation balance would be a<br />

systematic program to deliver orbiters with entry probes to all four giant planets <strong>in</strong> <strong>the</strong> solar system. The<br />

probes would determ<strong>in</strong>e <strong>the</strong> composition, cloud structures, <strong>and</strong> w<strong>in</strong>ds as a function of depth <strong>and</strong> location<br />

on each planet. They would be delivered by capable orbit<strong>in</strong>g spacecraft that provide remote sens<strong>in</strong>g of<br />

<strong>the</strong> cloud deck <strong>in</strong> visible light as well <strong>the</strong> near- <strong>and</strong> <strong>the</strong>rmal-<strong>in</strong>frared regimes, <strong>and</strong> would yield detailed<br />

gravitational measurements to constra<strong>in</strong> planetary <strong>in</strong>terior structure. 15<br />

The Galileo mission began this program at Jupiter. Indeed, Jupiter has been well studied by<br />

seven flyby missions, as well as by <strong>the</strong> Galileo spacecraft that spent almost 8 years <strong>in</strong> jovian orbit <strong>and</strong><br />

delivered an <strong>in</strong> situ atmospheric probe. Jupiter is also <strong>the</strong> target of <strong>the</strong> Juno mission, <strong>the</strong> top priority of<br />

<strong>the</strong> Giant Planets Panel <strong>in</strong> <strong>the</strong> last decadal survey. Juno will constra<strong>in</strong> H2O <strong>and</strong> possibly sense deep<br />

convective perturbations of <strong>the</strong> gravitational field. The Jupiter Europa Orbiter (JEO), NASA’s<br />

contribution to <strong>the</strong> proposed NASA-ESA Europa Jupiter <strong>System</strong> Mission might provide some<br />

confirmation of <strong>the</strong>rmal <strong>and</strong> visible albedo measurements taken by Cass<strong>in</strong>i <strong>and</strong> from Earth depend<strong>in</strong>g on<br />

f<strong>in</strong>al <strong>in</strong>strumentation. However, <strong>the</strong> selected orbit of JEO <strong>and</strong> <strong>the</strong> need to protect <strong>the</strong> craft will yield only<br />

limited <strong>in</strong><strong>for</strong>mation to supplement Juno’s determ<strong>in</strong>ation of gravitational moments <strong>and</strong> <strong>the</strong> nature of <strong>the</strong><br />

<strong>in</strong>ner magnetic field. Jupiter is our best-studied <strong>and</strong> best-understood analog <strong>for</strong> exoplanet <strong>for</strong>mation.<br />

Fur<strong>the</strong>r jovian studies would benefit most by <strong>the</strong> development of a more complete scientific<br />

underst<strong>and</strong><strong>in</strong>g of <strong>the</strong> o<strong>the</strong>r giant planets, <strong>for</strong> which far less is known. 16<br />

A Saturn probe coupled with Cass<strong>in</strong>i data (remote sens<strong>in</strong>g <strong>and</strong> gravitational <strong>in</strong><strong>for</strong>mation from its<br />

f<strong>in</strong>al phase) can test <strong>the</strong> He differentiation hypo<strong>the</strong>sis through measurement of <strong>the</strong> He abundance. Such a<br />

measurement by a Saturn entry probe would resolve a decades-old, fundamental question <strong>in</strong> solar system<br />

science. The probe would also provide atmospheric elemental <strong>and</strong> isotopic abundances, <strong>in</strong>clud<strong>in</strong>g<br />

methane abundances. Such measurements address <strong>for</strong>mation history <strong>and</strong> help to better constra<strong>in</strong><br />

atmospheric opacity <strong>for</strong> gas giant evolutionary model<strong>in</strong>g. 17<br />

An ice giant entry probe will likewise measure atmospheric elemental <strong>and</strong> isotopic abundances—<br />

hence prob<strong>in</strong>g <strong>for</strong>mation mechanisms—<strong>and</strong> aga<strong>in</strong> measure methane abundances <strong>and</strong> <strong>the</strong>rmal profiles<br />

necessary <strong>for</strong> ice giant evolutionary model<strong>in</strong>g. An ice-giant orbiter—provid<strong>in</strong>g high-precision bolometric<br />

<strong>and</strong> Bond-albedo measurements, phase functions, <strong>and</strong> mid- <strong>and</strong> far-<strong>in</strong>frared <strong>the</strong>rmal lum<strong>in</strong>osity—will<br />

provide significant advances <strong>in</strong> underst<strong>and</strong><strong>in</strong>g energy balance <strong>in</strong> ice giant atmospheres. An orbiter with<br />

ultraviolet capability can address <strong>the</strong> issue of <strong>the</strong> hot corona by observ<strong>in</strong>g <strong>the</strong> altitud<strong>in</strong>al extent of <strong>the</strong><br />

upper atmosphere. A mission comb<strong>in</strong><strong>in</strong>g an orbiter <strong>and</strong> a probe will revolutionize our underst<strong>and</strong><strong>in</strong>g of<br />

ice giant properties <strong>and</strong> processes, yield<strong>in</strong>g significant <strong>in</strong>sight <strong>in</strong>to <strong>the</strong>ir evolutionary history.<br />

Throughout <strong>the</strong> next decade, research <strong>and</strong> analysis support should be provided to <strong>in</strong>terpret<br />

spacecraft results from <strong>the</strong> gas giants <strong>and</strong> to cont<strong>in</strong>ue ongo<strong>in</strong>g <strong>the</strong>rmal <strong>and</strong> albedo observations of <strong>the</strong> ice<br />

giants. The latter is of particular importance because of <strong>the</strong> excruciat<strong>in</strong>gly long time between spacecraft<br />

visits: this necessitates regular observations from state-of-<strong>the</strong>-art Earth-based facilities to provide longterm<br />

context <strong>for</strong> <strong>the</strong> short-duration spacecraft encounters. 18<br />

PREPUBLICATION COPY—SUBJECT TO FURTHER EDITORIAL CORRECTION<br />

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