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

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EXPLORING THE GIANT PLANET’S ROLES IN PROMOTING<br />

A HABITABLE PLANETARY SYSTEM<br />

The solar system conta<strong>in</strong>s myriad objects—small <strong>and</strong> large—orbit<strong>in</strong>g <strong>the</strong> Sun, <strong>and</strong> <strong>the</strong>se bodies<br />

can directly affect <strong>the</strong> habitability of Earth. For example, large planetary impacts are an ongo<strong>in</strong>g process,<br />

not merely a historical fact. Observations of Jupiter make this very clear; witness <strong>the</strong> spectacular impact<br />

of D/Shoemaker-Levy 9 with Jupiter <strong>in</strong> 1994. The effects of <strong>the</strong> jovian collisions prompted studies of,<br />

<strong>and</strong> surveys <strong>for</strong>, potentially hazardous asteroids <strong>in</strong> near-Earth space. The surpris<strong>in</strong>g second collision of a<br />

body with Jupiter <strong>in</strong> 2009, followed by two more jovian impacts <strong>in</strong> 2010, underscores <strong>the</strong> hazards <strong>in</strong> <strong>the</strong><br />

<strong>in</strong>terplanetary environment.<br />

The Sun itself is highly variable, with potentially significant consequences. The explosive release<br />

of stored magnetic energy <strong>in</strong> <strong>the</strong> Sun’s atmosphere leads to extremely large solar “storms,” caus<strong>in</strong>g<br />

changes <strong>in</strong> emitted electromagnetic radiation at all energies, eject<strong>in</strong>g energetic particles, <strong>and</strong> enhanc<strong>in</strong>g<br />

<strong>the</strong> solar w<strong>in</strong>d at Earth. The most prom<strong>in</strong>ent examples of <strong>the</strong>ir manifestations <strong>in</strong>clude not only natural<br />

spectacles such as auroral displays, but also direct impacts on human activities such as catastrophic<br />

failures of electrical grids <strong>and</strong> spacecraft hardware. The aurorae of <strong>the</strong> Jupiter <strong>and</strong> Saturn provide<br />

important data po<strong>in</strong>ts <strong>in</strong> underst<strong>and</strong><strong>in</strong>g <strong>the</strong> propagation of <strong>the</strong>se storms across <strong>the</strong> solar system.<br />

Underst<strong>and</strong><strong>in</strong>g <strong>the</strong>se solar eruptions, <strong>and</strong> <strong>the</strong>ir propagation to Earth <strong>and</strong> beyond, plays an important role <strong>in</strong><br />

contemporary solar physics <strong>and</strong> has generated its own field of space wea<strong>the</strong>r.<br />

By study<strong>in</strong>g <strong>the</strong> giant planets <strong>in</strong> <strong>the</strong> context of processes that occur throughout <strong>the</strong> solar system,<br />

we ga<strong>in</strong> a deeper underst<strong>and</strong><strong>in</strong>g of how those processes play out here on Earth. This is illustrated with<br />

specific examples about energy balance, <strong>in</strong>teractions with <strong>the</strong> Sun’s magnetic field, <strong>and</strong> how <strong>the</strong> surfaces<br />

<strong>in</strong> giant planet systems are “wea<strong>the</strong>red.”<br />

Specific objectives associated with <strong>the</strong> goal of explor<strong>in</strong>g <strong>the</strong> giant planets’ role <strong>in</strong> craft<strong>in</strong>g a<br />

habitable planetary system <strong>in</strong>clude <strong>the</strong> follow<strong>in</strong>g:<br />

• Search <strong>for</strong> chemical evidence of planetary migration;<br />

• Explore <strong>the</strong> giant planets’ role <strong>in</strong> creat<strong>in</strong>g our habitable Earth via large impacts; <strong>and</strong><br />

• Determ<strong>in</strong>e <strong>the</strong> role of surface modification via smaller impacts.<br />

Subsequent sections exam<strong>in</strong>e each of <strong>the</strong>se objectives <strong>in</strong> turn, identifies important questions to be<br />

addressed <strong>and</strong> future <strong>in</strong>vestigations <strong>and</strong> measurements that could provide answers.<br />

Search <strong>for</strong> Chemical Evidence of <strong>Planetary</strong> Migration<br />

In <strong>the</strong> past, various models have been proposed <strong>for</strong> <strong>for</strong>mation of planetary systems <strong>in</strong> general <strong>and</strong><br />

specifically <strong>for</strong> <strong>the</strong> solar system. All <strong>the</strong>se models made basic assumptions concern<strong>in</strong>g condensation of<br />

planet-<strong>for</strong>m<strong>in</strong>g components <strong>and</strong> <strong>the</strong> manner <strong>in</strong> which <strong>the</strong>y were accumulated by <strong>the</strong> planets. In <strong>the</strong> last<br />

two decades, <strong>in</strong>creased comput<strong>in</strong>g power has led to rejection of some models <strong>and</strong> <strong>in</strong>creased support <strong>for</strong> a<br />

model <strong>in</strong> which Jupiter <strong>and</strong> Saturn <strong>in</strong>teracted to perturb <strong>the</strong> planets <strong>in</strong>to <strong>the</strong>ir current configuration. The<br />

degree to which <strong>the</strong> planets were <strong>for</strong>med by collisional impacts of volatile-bear<strong>in</strong>g bodies or collapse of<br />

gases onto larger bodies should have left beh<strong>in</strong>d evidence that can be found with<strong>in</strong> <strong>the</strong> compositional<br />

makeup of <strong>the</strong> surviv<strong>in</strong>g bodies. Thus, determ<strong>in</strong>ation of <strong>the</strong> chemical composition (D/H, o<strong>the</strong>r isotopic<br />

abundances, noble gases, water) will discrim<strong>in</strong>ate among models that will constra<strong>in</strong> <strong>in</strong>itial conditions <strong>and</strong><br />

illum<strong>in</strong>ate how <strong>the</strong> planets have evolved.<br />

The distribution of <strong>the</strong> heavy elements (atomic mass >4) as a function of distance from <strong>the</strong> Sun<br />

can provide strong constra<strong>in</strong>ts <strong>for</strong> discrim<strong>in</strong>at<strong>in</strong>g among <strong>the</strong>ories <strong>and</strong> dynamical models of solar system<br />

<strong>for</strong>mation <strong>and</strong> evolution. One of <strong>the</strong> predictions of <strong>the</strong> models is that <strong>the</strong> central core mass of <strong>the</strong> giant<br />

planets should <strong>in</strong>crease with distance from <strong>the</strong> Sun. This should result <strong>in</strong> a correspond<strong>in</strong>g <strong>in</strong>crease <strong>in</strong> <strong>the</strong><br />

abundances of <strong>the</strong> heavier elements. Currently <strong>the</strong> only element measured <strong>for</strong> all four planets is carbon,<br />

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

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