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Passage to a Ringed World - NASA's History Office

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field reverses direction across the<br />

tail’s plasma sheet (a thin sheet of<br />

plasma located approximately in the<br />

planet’s equa<strong>to</strong>rial plane, where currents<br />

flow and particles are accelerated.<br />

The process of reconnection and<br />

opening of field lines on the sunward<br />

side of the magne<strong>to</strong>sphere is thus balanced<br />

by reconnection that closes<br />

field lines in the magne<strong>to</strong>tail. The<br />

newly closed field lines contract back<br />

<strong>to</strong>ward the planet, pulling the plasma<br />

along and driving a circulation pattern,<br />

as shown in the figure below.<br />

The process of reconnection on the<br />

Sunward side of the magne<strong>to</strong>sphere<br />

is thus closely coupled <strong>to</strong> processes<br />

that occur in the magne<strong>to</strong>tail. These<br />

processes are known <strong>to</strong> be strongly<br />

SOLAR WIND CIRCULATION<br />

Large-scale circulation<br />

driven by the<br />

solar wind as it occurs<br />

at Earth. An<br />

analogous process<br />

occurs at Saturn. The<br />

orientations of magnetic<br />

field lines and<br />

plasma flows are<br />

shown. When the interplanetary<br />

magnetic<br />

field is oriented southward,<br />

as shown, field<br />

lines reconnect at the<br />

nose of the magne<strong>to</strong>pause<br />

and then<br />

again in the magne<strong>to</strong>tail,<br />

driving the<br />

flows described in<br />

the chapter text.<br />

affected by the changing conditions<br />

in the solar wind. At Earth, reconnection<br />

processes can give rise <strong>to</strong> large,<br />

erratic changes in the global configuration<br />

of the magne<strong>to</strong>sphere referred<br />

<strong>to</strong> as geomagnetic s<strong>to</strong>rms. Cassini’s<br />

MAPS instruments will investigate <strong>to</strong><br />

see if similar magne<strong>to</strong>spheric s<strong>to</strong>rms<br />

occur at Saturn.<br />

Voyager 1 made the first direct measurement<br />

of Saturn’s magne<strong>to</strong>tail,<br />

finding it <strong>to</strong> resemble its terrestrial<br />

and Jupiter counterparts. The magne<strong>to</strong>tail<br />

was detected <strong>to</strong> be roughly<br />

40 R in diameter at a distance 25 R S S<br />

downstream; it may extend hundreds<br />

of Saturn radii in the downstream solar<br />

wind. Understanding the processes<br />

that occur in the magne<strong>to</strong>tail is<br />

fundamental <strong>to</strong> understanding overall<br />

Solar Wind Reconnection<br />

magne<strong>to</strong>spheric dynamics; coordinated<br />

measurements by the MAPS instruments<br />

during the deep tail orbits<br />

planned for the Cassini <strong>to</strong>ur will contribute<br />

<strong>to</strong> that understanding. In turn,<br />

by understanding overall magne<strong>to</strong>spheric<br />

dynamics, scientists will gain<br />

insight in<strong>to</strong> how Saturn’s magne<strong>to</strong>sphere<br />

harnesses energy from the solar<br />

wind.<br />

Current Magne<strong>to</strong>spheric Systems<br />

Various large-scale current systems<br />

exist in Saturn’s magne<strong>to</strong>sphere due<br />

<strong>to</strong> the collective motions of charged<br />

particles. Cross-tail currents flow from<br />

dusk <strong>to</strong> dawn in the plasma sheet located<br />

near the center of the magne<strong>to</strong>tail.<br />

An equa<strong>to</strong>rial ring current<br />

dis<strong>to</strong>rts the magnetic field from its di-<br />

Magne<strong>to</strong>pause<br />

Tailward Flow<br />

Reconnection<br />

A SPHERE OF INFLUENCE 71

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