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Passage to a Ringed World - NASA's History Office

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Sources of particles<br />

in Saturn’s<br />

magne<strong>to</strong>sphere.<br />

68 PASSAGE TO A RINGED WORLD<br />

Most of what we know about Saturn’s<br />

magne<strong>to</strong>sphere comes from the brief<br />

visits by Pioneer 11 and Voyagers 1<br />

and 2, but remote observations by the<br />

Hubble Space Telescope and other<br />

spacecraft have also provided us with<br />

intriguing information.<br />

Magne<strong>to</strong>spheric Particle Sources<br />

Saturn has a variety of sources for the<br />

particles in its magne<strong>to</strong>sphere. Particles<br />

can escape from any moon, ring<br />

or dust particle surface, or they can<br />

be “sputtered” off by energetic particles<br />

or even micrometeoroid impacts.<br />

The primary particle sources are<br />

thought <strong>to</strong> be the moons Dione and<br />

Tethys. But, the solar wind, iono-<br />

Main Ring<br />

F-Ring<br />

Mimas<br />

Enceladus<br />

Tethys<br />

G-Ring E-Ring<br />

sphere, rings, Saturn’s atmosphere,<br />

Titan’s atmosphere and the other icy<br />

moons are sources as well. Recent<br />

Hubble Space Telescope results show<br />

large numbers of neutral hydrogen<br />

a<strong>to</strong>ms (the neutral hydrogen cloud in<br />

the illustration above) throughout the<br />

magne<strong>to</strong>sphere that probably come<br />

from a number of these sources. It has<br />

even been proposed that water ions<br />

and molecules may form a dense<br />

“ionosphere” above Saturn’s rings.<br />

Recent Hubble Space Telescope results<br />

show large numbers of neutral<br />

hydrogen a<strong>to</strong>ms throughout the magne<strong>to</strong>sphere<br />

that probably come from<br />

a number of the sources mentioned.<br />

Determining the relative importance<br />

of the varied sources in different<br />

parts of Saturn’s space environment<br />

is a prime objective for the Magne<strong>to</strong>spheric<br />

and Plasma Science (MAPS)<br />

instruments aboard the Cassini<br />

spacecraft.<br />

Neutral particles can escape from<br />

any moon, ring or dust particle sur-<br />

Dione<br />

H 2 O<br />

Rhea<br />

face — or they can be “sputtered”<br />

off by energetic particles or even<br />

micrometeoroid impacts. When<br />

these particles become ionized, they<br />

can excite electromagnetic waves<br />

with a frequency that can be used<br />

<strong>to</strong> determine their type. The icy rings<br />

absorb the energetic particles inward<br />

of the moon Mimas. Energetic parti-<br />

cles can be created by processes<br />

within the magne<strong>to</strong>sphere or they<br />

can leak in from the solar wind.<br />

These and many other magne<strong>to</strong>spheric<br />

phenomena were seen by<br />

the three earlier spacecraft.<br />

The mysterious “spokes” in the rings<br />

of Saturn, clearly seen in Voyager<br />

images, are probably caused by electrodynamic<br />

interactions between the<br />

tiny charged dust particles in the<br />

rings and the magne<strong>to</strong>sphere. Auroras,<br />

which exist on Saturn as well as<br />

Earth, are produced when trapped<br />

charged particles precipitating from<br />

the magne<strong>to</strong>sphere collide with atmospheric<br />

gases.<br />

Neutral<br />

Hydrogen Cloud<br />

Titan<br />

Despite many exciting discoveries,<br />

many more questions about the physical<br />

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

remain unanswered. This<br />

chapter examines the current state<br />

of knowledge about Saturn’s magne<strong>to</strong>sphere<br />

and discusses the observations<br />

we expect <strong>to</strong> make with<br />

Cassini’s instruments and the knowledge<br />

we expect <strong>to</strong> gain from forthcoming<br />

explorations.

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