Vision and Voyages for Planetary Science in the - Solar System ...
Vision and Voyages for Planetary Science in the - Solar System ...
Vision and Voyages for Planetary Science in the - Solar System ...
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• Venus In Situ Explorer<br />
• South Pole-Aitken Bas<strong>in</strong> Sample Returm<br />
Venus In Situ Explorer<br />
VISE’s importance was reaffirmed <strong>in</strong> <strong>the</strong> NRC’s Open<strong>in</strong>g New Frontiers <strong>in</strong> <strong>Solar</strong> <strong>System</strong><br />
Exploration. 22 The rationale <strong>for</strong> VISE is that many crucial analyses of Venus cannot be obta<strong>in</strong>ed from<br />
orbit <strong>and</strong> <strong>in</strong>stead require <strong>in</strong> situ <strong>in</strong>vestigations. Sample return appears beyond current technology, <strong>and</strong><br />
Venus’s thick atmosphere limits <strong>the</strong> primary tools <strong>for</strong> surface <strong>in</strong>vestigations from orbit to radar, radio<br />
science, gravity, <strong>and</strong> a few w<strong>in</strong>dows <strong>in</strong> near-<strong>in</strong>frared wavelengths. The science mission objectives <strong>for</strong><br />
VISE from <strong>the</strong>se previous reports are as follows:<br />
• Underst<strong>and</strong> <strong>the</strong> physics <strong>and</strong> chemistry of Venus’s atmosphere, especially <strong>the</strong> abundances of<br />
its trace gases, sulfur, light stable isotopes, <strong>and</strong> noble gas isotopes;<br />
• Constra<strong>in</strong> <strong>the</strong> coupl<strong>in</strong>g of <strong>the</strong>rmochemical, photochemical, <strong>and</strong> dynamical processes <strong>in</strong><br />
Venus’s atmosphere <strong>and</strong> between <strong>the</strong> surface <strong>and</strong> atmosphere to underst<strong>and</strong> radiative balance, climate,<br />
dynamics, <strong>and</strong> chemical cycles;<br />
• Underst<strong>and</strong> <strong>the</strong> physics <strong>and</strong> chemistry of Venus’s crust;<br />
• Underst<strong>and</strong> <strong>the</strong> properties of Venus’s atmosphere down to <strong>the</strong> surface <strong>and</strong> improve our<br />
underst<strong>and</strong><strong>in</strong>g of Venus’s zonal cloud-level w<strong>in</strong>ds;<br />
• Underst<strong>and</strong> <strong>the</strong> wea<strong>the</strong>r<strong>in</strong>g environment of <strong>the</strong> crust of Venus <strong>in</strong> <strong>the</strong> context of <strong>the</strong> dynamics<br />
of <strong>the</strong> atmosphere <strong>and</strong> <strong>the</strong> composition <strong>and</strong> texture of its surface materials; <strong>and</strong><br />
• Look <strong>for</strong> planetary scale evidence of past hydrological cycles, oceans, <strong>and</strong> life <strong>and</strong> <strong>for</strong><br />
constra<strong>in</strong>ts on <strong>the</strong> evolution of <strong>the</strong> atmosphere of Venus.<br />
Achiev<strong>in</strong>g all of <strong>the</strong>se objectives represents a flagship-class <strong>in</strong>vestment, 23 but achiev<strong>in</strong>g a<br />
majority is considered feasible <strong>in</strong> <strong>the</strong> New Frontiers Program. 24<br />
In <strong>the</strong> 2003 decadal survey, <strong>the</strong> long-term goal was extraction <strong>and</strong> return to Earth of samples<br />
(solid <strong>and</strong> gas) from <strong>the</strong> Venus surface, clearly a flagship-class mission, <strong>and</strong> VISE was considered <strong>in</strong><br />
terms of its contribution to this sample return. The 2008 NRC report suggested that VISE not be tied to<br />
Venus sample return, given <strong>the</strong> huge (<strong>and</strong> so-far unanswered) technical challenges posed by <strong>the</strong> latter.<br />
VISE-like missions do, however, provide <strong>the</strong> rare opportunities <strong>for</strong> technical demonstrations <strong>in</strong> <strong>the</strong> Venus<br />
near-surface environment, <strong>and</strong> <strong>in</strong>clusion of demonstration technologies on a VISE mission would be<br />
justified (on a non-<strong>in</strong>terference, non-critical-path basis).<br />
South Pole–Aiken Bas<strong>in</strong> Sample Return<br />
The exploration <strong>and</strong> sample return from <strong>the</strong> Moon’s South Pole-Aitken (SPA) bas<strong>in</strong> is among <strong>the</strong><br />
highest priority activities <strong>for</strong> solar system science. The mission’s high priority stems from its role <strong>in</strong><br />
address<strong>in</strong>g multiple science objectives outl<strong>in</strong>ed <strong>in</strong> this report, <strong>in</strong>clud<strong>in</strong>g underst<strong>and</strong><strong>in</strong>g <strong>the</strong> <strong>in</strong>terior of <strong>the</strong><br />
Moon <strong>and</strong> impact history of <strong>the</strong> solar system. Though recent remote-sens<strong>in</strong>g missions provide much<br />
valuable new data from orbit about <strong>the</strong> diversity of materials <strong>and</strong> <strong>the</strong> geophysical context of this important<br />
bas<strong>in</strong>, achiev<strong>in</strong>g <strong>the</strong> highest-priority science objectives requires precision of age measurements to better<br />
than ±20 million years <strong>and</strong> accuracy of trace elemental compositions to <strong>the</strong> parts-per-billion level, which<br />
is only achievable via sample return. The pr<strong>in</strong>cipal scientific reasons <strong>for</strong> undertak<strong>in</strong>g a South Pole-Aitken<br />
Bas<strong>in</strong> Sample Return mission are as follows:<br />
• Determ<strong>in</strong>e <strong>the</strong> chronology of bas<strong>in</strong>-<strong>for</strong>m<strong>in</strong>g impacts <strong>and</strong> constra<strong>in</strong> <strong>the</strong> period of late heavy<br />
bombardment <strong>in</strong> <strong>the</strong> <strong>in</strong>ner solar system, <strong>and</strong> thus address fundamental questions of <strong>in</strong>ner solar system<br />
impact processes <strong>and</strong> chronology;<br />
PREPUBLICATION COPY—SUBJECT TO FURTHER EDITORIAL CORRECTION<br />
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