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Saturn

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All three layers are thicker than on Jupiter. Atmospheric Coloration. Longitudinal Bands ... Realized in 1659 (Christian Huygens) to be a flat ring system ... – PowerPoint PPT presentation

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Title: Saturn


1
Saturn
2
Bulk Properties
  • Radius 9.5 Earth radii
  • Mass 95 Earth masses
  • Density 0.687 g/cm3
  • Semi-major Axis 9.5 A.U. (9.0-10.0)
  • Orbital Period 29.5 years
  • Rotational Period 10.5 hours
  • Differential rotation
  • Oblate spheroid (even more than Jupiter)

3
Saturns Atmosphere
  • Composition
  • 92 Hydrogen, 7 Helium
  • Trace amounts of methane and ammonia
  • Layers
  • Ammonia clouds
  • NH4HS clouds
  • water clouds
  • All three layers are thicker than on Jupiter

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Atmospheric Coloration
  • Longitudinal Bands
  • Not as prominent as on Jupiter
  • Due to thickness of the outer layer of clouds
  • Weather
  • Zonal flow Eastward in the zones and Westward in
    the belts
  • Very fast winds (1500km/hr)
  • Helium precipitation
  • A light shower of liquid helium constantly
    falling from the lower atmosphere toward the
    interior

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Saturns Interior
  • Very similar to Jupiter
  • Large rocky core
  • Liquid metallic hydrogen
  • Liquid molecular hydrogen
  • Hydrogen/Helium atmosphere
  • Magnetic field strength intermediate between
    Earth and Jupiter
  • Large enough to contain the ring system and the
    innermost 16 moons (about the orbit of Titan)

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Saturns Rings
  • First observed by Galileo in 1610
  • Thought Saturn was a triple planet as it
    appeared to have bumps or ears
  • Realized in 1659 (Christian Huygens) to be a flat
    ring system
  • First ring feature (a dark band in the rings)
    found in 1675 by Giovanni Cassini

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Composition
  • Small rocky and icy bodies
  • Most about the size of a softball
  • The ring system is only a few tens of meters
    thick
  • Not one big ring, but several rings
  • Original designations from outside in.
  • A-ring (Contains the Encke gap)
  • Cassini division
  • B-ring
  • C-ring
  • Other rings discovered by Pioneer and Voyager
    probes
  • Inside C-ring is the D-ring
  • Outside A-ring is the F-ring and the E-ring
    (faint and very far)

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How did the rings form?
  • Tidal forces increase nearer the planet
  • If a body gets close enough that the tidal forces
    exceed the gravitational forces holding the
    object together, it breaks apart
  • The distance at which this happens is called the
    Roche Limit
  • It is believed that a moon was torn apart by
    tidal forces and formed the rings

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Ring Maintenance
  • Orbital Resonance
  • A particle orbiting in the Cassini Division has
    an orbital period exactly half that of Saturns
    innermost major moon (Mimas)
  • The extra gravitational forces present at this
    distance stretches the original circular orbit
    into an elliptical one
  • This eventually clears the area of particles,
    resulting in a low density gap

17
Ring Maintenance
  • Shepherd Satellites
  • Small moons that orbit on either side of a
    ringlet
  • The F-ring is surrounded by the orbits of
    Prometheus and Pandora
  • Keeps the ring tightly confined in a narrow orbit
  • Moonlets
  • Small moons that sweep up ring debris and create
    small gaps
  • Pan creates the Encke gap

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