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Lecture 12
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Key Words liquid metallic hydrogen noble gases oblate, oblateness
plasma tidal force
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Outline Jupiter and Saturn Orbit Surface Atmosphere Rings Moons
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It is difficult to see!
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Inferior planets superior planets
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A planet’s synodic period is measured with respect to the Earth and the Sun (for example, from one opposition to the next)
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Periods Rotational Orbital Sidereal Synodic
Measured with respect to something that is not rotating or orbiting
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Question Which is longer, Jupiter’s synodic or orbital period?
Which is longer, Jupiter’s synodic or Saturn’s synodic period? Guess Jupiter’s and Saturn’s synodic period.
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Kepler’s Third Law P2 = a3 P = planet’s sidereal period, in years
a = planet’s semimajor axis, in AU
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Long orbital periods of Jupiter and Saturn cause favorable viewing times to shift
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The best time to observe Saturn from Earth is when it is
at opposition and it is midnight at your location on Earth. at opposition and it is sunset or sunrise at your location on Earth. at conjunction and it is midnight at your location on Earth. at conjunction and it is sunset or sunrise at your location on Earth. at opposition and it is just before sunrise at your location on Earth.
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Outline Jupiter and Saturn Orbit Surface Atmosphere Rings Moons
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How to get Oblate hoop
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What happens to ornaments when hoop is spun?
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The oblateness of Jupiter and Saturn reveals their rocky cores
Jupiter probably has a rocky core several times more massive than the Earth The core is surrounded by a layer of liquid “ices” (water, ammonia, methane, and associated compounds)
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The oblateness of Jupiter and Saturn reveals their rocky cores
On top of this is a layer of helium and liquid metallic hydrogen and an outermost layer composed primarily of ordinary hydrogen and helium Saturn’s internal structure is similar to that of Jupiter, but its core makes up a larger fraction of its volume and its liquid metallic hydrogen mantle is shallower than that of Jupiter
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Metallic hydrogen inside Jupiter and Saturn endows the planets with strong magnetic fields
Jupiter and Saturn have strong magnetic fields created by currents in the metallic hydrogen layer Jupiter’s huge magnetosphere contains a vast current sheet of electrically charged particles Saturn’s magnetic field and magnetosphere are much less extensive than Jupiter’s
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Jupiter and Saturn have extensive magnetospheres
The Jovian magnetosphere encloses a low-density plasma of charged particles The magnetosphere exists in a delicate balance between pressures from the plasma and from the solar wind When this balance is disturbed, the size of the magnetosphere fluctuates drastically
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Synchrotron Radiation
Charged particles in the densest portions of Jupiter’s magnetosphere emit synchrotron radiation at radio wavelengths
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Auroras on Jupiter and Saturn are caused by
charged particles from the magnetosphere colliding with molecules in the upper atmosphere. ionized hydrogen. ionized helium. tidal interactions with the largest moons. gas circulating at the poles.
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Outline Jupiter and Saturn Orbit Surface Atmosphere Rings Moons
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Atmospheres gravity and escape velocity
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Atmospheres gravity and escape velocity
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Atmospheres The visible “surfaces” of Jupiter and Saturn are actually the tops of their clouds
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Atmospheres The rapid rotation of the planets twists the clouds into dark belts and light zones that run parallel to the equator
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The chemical composition of Jupiter and Saturn is difficult to measure
The chemical composition of Jupiter and Saturn is difficult to measure. Why?
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Atmospheres The outer layers of both planets’ atmospheres show differential rotation The equatorial regions rotate slightly faster than the polar regions
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Atmospheres For both Jupiter and Saturn, the polar rotation rate is nearly the same as the internal rotation rate
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Spacecraft images show remarkable activity in the clouds of Jupiter and Saturn
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Storms Both Jupiter and Saturn emit more energy than they receive from the Sun Presumably both planets are still cooling The colored ovals visible in the Jovian atmosphere represent gigantic storms Some, such as the Great Red Spot, are quite stable and persist for many years
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Storms in Saturn’s atmosphere seem to be shorter-lived
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The internal heat of Jupiter and Saturn has a major effect on the planets’ atmospheres
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A space probe has explored Jupiter’s deep atmosphere
There are presumed to be three cloud layers in the atmospheres of Jupiter and Saturn The reasons for the distinctive colors of these different layers are not yet known The cloud layers in Saturn’s atmosphere are spread out over a greater range of altitude than those of Jupiter, giving Saturn a more washed-out appearance Saturn’s atmosphere contains less helium than Jupiter’s atmosphere This lower abundance may be the result of helium raining downward into the planet Helium “rainfall” may also account for Saturn’s surprisingly strong heat output
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Spacecraft images show remarkable activity in the clouds of Jupiter and Saturn
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In the news: Hurricane on Saturn?
Hurricane-like vortex at Saturn's south pole, where the vertical structure of the clouds is highlighted by shadows. Such a storm, with a well-developed eye ringed by towering clouds, is a phenomenon never before seen on another planet.
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Both Jupiter and Saturn emit more energy than they receive from the Sun. What does this tell us?
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Jupiter radiates more energy into space than it receives from the Sun
Jupiter radiates more energy into space than it receives from the Sun. What is the primary source of the excess energy that Jupiter radiates? Decay of radioactive materials in Jupiter's core Tidal forces from Jupiter's moons Jupiter is still contracting, and the contraction releases energy Jupiter's rotation is slowing down dramatically, and this slowdown releases energy All of the above are the energy sources
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What can you say about these planets?
Figure 7-11 Planet Size and Cratering Of these two hypothetical planets, the smaller one (#2) has less volume and less internal heat, as well as less surface area from which to radiate heat into space. But the ratio of surface area to volume is greater for the smaller planet. Hence, the smaller planet will lose heat faster, have a colder interior, and be less geologically active. It will also have a more heavily cratered surface, since it takes geologic activity to erase craters. What can you say about these planets?
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If Jupiter and Saturn formed at the same time, which should be emitting more heat?
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Outline Jupiter and Saturn Orbit Surface Atmosphere Rings Moons
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Why can’t the rings be solid?
Roche limit
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Link
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Something is Fishy How can a planet be solid?
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Pebbles, snowballs and boulder size
How was this determined?
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Earth-based observations reveal three broad rings encircling Saturn
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Saturn is circled by a system of thin, broad rings lying in the plane of the planet’s equator
This system is tilted away from the plane of Saturn’s orbit, which causes the rings to be seen at various angles by an Earth-based observer over the course of a Saturnian year
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Saturn’s rings are composed of numerous icy fragments, while Jupiter’s rings are made of small rocky particles The principal rings of Saturn are composed of numerous particles of ice and ice-coated rock ranging in size from a few micrometers to about 10 m Jupiter’s faint rings are composed of a relatively small amount of small, dark, rocky particles that reflect very little light
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Most of its rings exist inside the Roche limit of Saturn, where disruptive tidal forces are stronger than the gravitational forces attracting the ring particles to each other Each of Saturn’s major rings is composed of a great many narrow ringlets
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Saturn’s rings consist of thousands of narrow, closely spaced ringlets
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Saturn’s inner satellites affect the appearance and structure of its rings
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The faint F ring, which is just outside the A ring, is kept narrow by the gravitational pull of shepherd satellites
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Outline Jupiter and Saturn Orbit Surface Atmosphere Rings Moons
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Preview Already discussed influence on Saturn’s rings.
Jupiter’s moons are even more interesting
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