skip navigation
Astronomy 171
Solar System Astronomy
Prof. Paul Martini

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.

[ Return to the Astronomy 171 Main Page | Unit 6 Page ]


Updated: 2007 February 24 Copyright © Paul Martini All Rights Reserved.