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Astronomy 171
Solar System Astronomy
Prof. Paul Martini
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Lecture 35: Massive Jupiter
Key Ideas:
- Jupiter is the largest of the Planets
- Prototype Gas Giant Planet
- Jupiter has many moons and a faint ring
- Atmosphere and Clouds
- Colored belts and zones
- Great red spot
- Gaseous atmosphere of Hydrogen and Helium
- Internal Structure
- Radiates more energy than it gets from the Sun
- Rocky inner core, liquid metallic outer core
Spacecraft to Jupiter
- Fly-bys:
- Pioneer 10 and 11 (1973 and 1974)
- Voyager 1 and 2 (1979)
- Ulysses (1992)
- Cassini (2001, while enroute to Saturn)
- Orbiters:
- Galileo (arrived Dec 1995, deliberately crashed into Jupiter in 2003)
- Dropped an atmospheric probe in Dec 1995
Jupiter is a Giant Gas Planet
- No solid surface
- Deep, heavy hydrogen and helium atmosphere
- Rock and ice core
- Rapidly rotating
- Rotates once every 9 hours and 50 minutes
- Measured using its magnetic field
- Flattened at the poles:
- Equatorial Radius: 71,492 km
- Polar Radius: 66,854 km (6.5% flattening)
63 Moons of Jupiter
- 4 Galilean moons
- Large (>3000 km)
- Spherical
- Differentiated
- 59 small moons
- Small (<200 km)
- Irregular in shape
- Undifferentiated
Jupiter's Dusty Rings
- Jupiter has faint, dusty rings:
- Made of micron-sized dark dust particles
- Total mass is < 10-12 MEarth
- Ring material may have been knocked off the moons of Jupiter or captured from comets
Atmosphere of Jupiter
- Composition:
- 86.4% H2 (Molecular Hydrogen)
- 13.6% He (Helium)
- <0.1% H2O (Water)
- 0.21% CH4 (Methane)
- 0.07% NH3 (Ammonia)
- 0.008% H2S (Hydrogen Sulfide)
Atmospheric Probe
- Released by the Galileo mission in December 1995
- Survived 200km into the atmosphere, until crushed by high pressure
- Relatively constant wind speed
- Measured the chemistry of the atmosphere
- Surprisingly little water
- High abundance of Xe, Ar, Kr
Clouds of Jupiter
- What we see are the tops of the clouds
- Crystals of ammonia, methane, and water ices
- Average temperatures is 100 - 140 K
- Atmosphere is divided into latitudinal bands:
- Dark Belts
- Bright Zones
- Cyclonic and Anti-Cyclonic storms
- The detailed chemistry of the colorful clouds is still not well understood
Belts and Zones of Jupiter
- Belts: high pressure and low temperature
- Gaps in high clouds, view lower atmosphere
- Colors due to complex organics and polysulfides
- Zones: low pressure, low temperature
- Regions of cold, high ice clouds
Cyclonic Storms?
- Strong winds at the belt/zone boundaries:
- Wind speeds up to 400 km/hr
- Blow east-to-west or west-to-east, alternating between belts/zones
- Some storms persist for centuries
Internal Energy
- Jupiter radiates 2.5x more energy than it receives from the Sun
- Slowly contracts under its own weight
- Releases gravitational energy that heats up the interior
- Explains constant wind speed in lower atmosphere
- This heat powers Jupiter's weather
Jupiter's Magnetic Field
- Circulating currents in the metallic hydrogen "mantle" of Jupiter generates a powerful magnetic field
- Strongest planetary magnetic field
- Tilted by ~9.6 degrees from the rotation axis
- Co-rotates with the planet's interior (~9 hours, 56 minutes)
- Generates energetic radio emission (one of the brightest radio sources in the sky)
- Ionized gas torus linked to the moon Io
Jupiter is not a failed star
- Jupiter resembles the Sun in composition, but it is not a "failed star"
- Formed from a rocky core that gathered hydrogen, helium, and volatiles from the surrounding proto-solar nebula
- Inner core is solid (rock and ice)
- Had a very different formation history than that of a small star
- The smallest stars are 12x larger
See A Note about Graphics to learn
why some of the graphics shown in the lectures are not reproduced with
these notes.
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Updated: 2007 February 24
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