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Jupiter Astronomy 311 Professor Lee Carkner Lecture 17
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Jupiter’s Great Red Spot is best described as,
An impact feature An eruption of water ice A hurricane-like storm A large cloud that absorbs red light The shadow of the moon Io
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Which best describes the surface of the typical gas giant moon?
Rocky Covered with volcanoes Enveloped by a thick atmosphere Smooth with few craters Icy
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The atmospheres of the gas giants are made of,
Helium with hydrogen clouds Hydrogen with clouds made of volatiles Carbon dioxide Oxygen and water vapor Unknown chemicals
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The rings of the gas giants are made of,
Very small dust grains Very bright icy grains Pieces of a moon that exploded Either small dark or large bright particles Small moons, about 1 km in size
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Jupiter -- King of the Gods
Jupiter is also “King of the Planets” due to its size
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Viewing Jupiter from Earth
Is very bright from Earth In opposition every 13 months Can clearly see cloud patterns, Great Red Spot and 4 largest moons even with small telescope
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Jupiter Facts Size: Orbit: 5.2 AU
Description: large, gaseous, many large satellites
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Viewing Jupiter from Space
Currently observed by Hubble Space Telescope The Galileo spacecraft ended its mission in 2003 Dropped a probe through the atmosphere
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Galileo’s Atmosphere Probe
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Galileo Atmosphere Probe
Launched from the Galileo spacecraft on Dec 7, 1995 Lasted for 1 hour and got down to 130 km below the tops of the clouds before the high temperature and pressure killed the electronics
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Shoemaker-Levy 9 Passed too close to Jupiter and was torn apart by tidal forces Each piece created a huge fireball Spectra of impacts reveals composition of deeper layers of atmosphere
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Convection Produced by convection
Hot material rises and cooler material sinks Jupiter has the most prominent clouds and belts of any planet Because it has the most internal energy
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Belts in Jupiter’s Atmosphere
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Jupiter’s Rotation Jupiter has a rotation period of about 10 hours
This rapid rotation shapes the belts and zones into oppositely circulating bands equator rotates faster than the poles this is because Jupiter is not a solid body
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Structure of Jupiter’s Atmosphere
Infrared, radio and Galileo probe observations reveal 3 cloud layers Ammonium hydrosulfide (NH4SH) The color of the layers depends on depth Brown -- White -- middle layer Red -- Not all layers are found in all regions Galileo found no water
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Structure of Jupiter’s Atmosphere
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Spots and Ovals They are rapidly rotating cloud features (storms)
Some are very long lived Some spots are white or brown Brown ovals may be holes to the deeper, hotter, inner atmosphere
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Interlude Gravity Every object in the solar system pulls on every other due to gravity This can cause perturbations in orbits We can use a modified version of this equation which shows the relative force a planet exerts: F=M/D2
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Jupiter’s Interior Small core of rock and ice (about the size of the Earth) Liquid metallic hydrogen outer core (40-50,000 km thick) Hydrogen gas layer 10-20,000 km thick
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The Interior of Jupiter
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Rings Jupiter’s rings were discovered by Voyager
May be formed from material chipped off of 4 small inner moons by impacts
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Diagram of Jupiter’s Rings and Inner Moons
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Jupiter’s Moons Jupiter has a planetary system of its own
Jupiter has 4 of the 7 large moons of the solar system
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Jupiter’s Magnetosphere
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Jupiter’s Magnetosphere
The magnetic field forms a magnetosphere about 200 times larger than Jupiter itself Also contains: a hot, thin, rapidly changing plasma rapidly moving changed particles
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Next Time Chapter
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Summary Jupiter is the largest planet
Its strong gravity influence the motions of the rest of the solar system Rotates rapidly and differentially Explored by Voyager, HST, Galileo, and a comet impact
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Summary: Atmosphere Explored by telescopes, Galileo probe and comet impact Clouds are composed of ammonia and sulfur compounds Clouds form bands of material moving in opposite directions Spots and ovals are storms which can occur at different altitudes and can be long lived Heat from Jupiter’s interior and rotation drives motions
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Summary: Jupiter From the Outside In
Satellites: out to ~24 million km Magnetosphere: out to ~15 million km Rings: out to ~200,000 km Atmosphere: out to ~70,000 km Liquid metallic hydrogen: out to ~50,000 km Rock/Ice core: out to ~20,000 km
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