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33 Cards in this Set

  • Front
  • Back

Jovian Planets

large, massive low-density worlds in the outer solar system


(Jupiter, Saturn, Uranus, Neptune)


have extensive satellite systems and moons (regular/irregular)

Belt-zone circulation

cloud belts parallel to the planets equator

Liquid Giants

Jupiter and Saturn are composed mostly of liquid metallic hydrogen

Ice Giants

Uranus and Neptune are abundant in solid water

Regular Satellites

large, close to parent planet, move in prograde direction (with the rest of the solar system)


Irregular Satellites

small, far from parent planet, and have high orbital inclinations


Jupiter

core made of heavy elements surrounded by a deep mantel of liquid metallic hydrogen


-large and strong magnetic field

Magnetosphere

around Jupiter; traps high-energy particles from the sun to form intense radiation belts

Atmosphere (Jupiter)

-three layers of clouds formed of hydrogen-rich molecules


-cloud layers are located at certain temperatures within the atmosphere


-cloud stripes parallel to equator are light/dark

Jupiter atmosphere cloud stripes

1. light-colored, high-pressure regions of rising gas


2. darker belts, lower-pressure areas of sinking gas

Spots in Jupiter's atmosphere

includes the Great Red Spot, are circulation weather patterns

Jupiter's Moons

-Galilean moons


-linked together in orbital resonances


-Io, Europa, Ganymede

Io (Jupiters Moon)

active volcanoes, orbits Jupiter 4 times

Europa (Jupiters Moon)

smooth ice and cracks, orbits Jupiter 2 times

Ganymede (Jupiters Moon)

grooved terrain, orbits Jupiter once

Jupiter's ring

composed of small particles that are bright when illuminated from behind (forward scattering)

Roche limit

distance from a planet within which the tidal stress can destroy or prevent one from forming (Jupiter's ring lies within Jupiter's Roche limit)

Saturn

-less dense than water


-contains a small core with less metallic hydrogen than Jupiter, therefore magnetic field is 20 times weaker


-moons are icy and mostly heavily cratered

Titan (Saturn's moon)

Saturn's largest moon; cold, cloudy nitrogen atmosphere


(so cold that gas molecules do not travel fast enough to escape)

Enceladus (Saturn's moon)

has a light surface with some uncratered regions

Saturns rings

composed of icy particles ranging in size from boulders to dust


-composition and brightness of the rings particles vary


-grooves in the rings can be produced by orbital resonances, or waves, that propagate through the rings caused by moons near or within the rings

Shephard satellites

the gravitational effect of small moons; can cause narrow rings and sharp ring edges

Jovian planets rings

cant be material left over from the formation of the planet


rings are replenished occasionally with material produced by meteoroids, asteroids, and comets colliding with moons

Uranus

-1/3 diameter of Jupiter, 1/20 as massive


-internal pressure cannot produce liquid hydrogen


-heavy-element core, mantle of solid or slushy ice and rocky material below a hydrogen-rich atmosphere


-atmosphere is almost featureless at visible wavelengths (pale blue color is caused by traces of methane which absorbs red light)


-rotates on its side (possibly due to major impact or tidal interactions with other planets during its early history)


-larger moons are icy and heavily cratered

Ovoids

grooves on Miranda, the innermost moon, caused by internal heat driving convection in the icy mantle

Occultations

the passage of the planet in front of a star during which the rings momentarily blocked the stars light


(how the rings of Uranus were discovered)

Rings of Uranus

narrow hoops of ice with traces of methane confined by shepherd satellites

Neptune

-ice giant with no liquid hydrogen


-has heat flowing from its interior


-atmosphere is rich in hydrogen and colored blue by traces of methane

Nereid (Neptunes Moon)

far off and follows a large elliptical orbit

Triton (Neptunes Moon)

-orbits backwards


-icy with a thin atmosphere and frosty polar caps


-smooth areas suggest past geological activity


-dark smudges mark the location of active nitrogen geysers

Neptunes rings

made up of icy particles in narrow hoops and contains arcs produced by the gravitational influence of one or more moons

Pluto

-small world with 3 moons, one of which, Charon, is quite large in relation to Pluto


-mostly rock with a substantial amount of ice


-redefined as a dwarf planet


-member of a family of Kuiper belt objects orbiting beyond Neptune

Plutinos

Kuiper belt objects that follow orbits like Pluto that have an orbital resonance with Neptune