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© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
The Jovian Planets
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
The Jovian planets are
gas giants -
much larger than Earth
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
Sizes of Jovian Planets
• Planets get larger as
they get more massive
• up to a point...
• Planets more massive
than Jupiter are
expected to shrink.
• There comes a point
where gravity wins:
adding more mass
causes contraction.
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
Jovian Planet Composition
• Jupiter and Saturn
— Mostly H and He gas
— these are the most common elements in the Universe
– “Gas Giants”
• Uranus and Neptune
— Mostly hydrogen compounds: water (H2O),
methane (CH4), ammonia (NH3)
— Some H, He, and rock
— “Ice Giants”
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
Interiors of Jovian Planets
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
Inside Jupiter
• High pressure inside
of Jupiter causes the
phase of hydrogen
to change with
depth.
• Hydrogen acts like a
metal at great depths
because its electrons
move freely.
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
Inside Jupiter
• The core is thought
to be made of rock,
metals, and
hydrogen
compounds.
• The core is about
the same size as
Earth but 10 times
as massive.
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
Comparing Jovian Interiors
• Models suggest that cores of jovian planets have
similar composition.
• Lower pressures inside Uranus and Neptune mean no
metallic hydrogen.
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
Jupiter’s Atmosphere
• Hydrogen compounds in
Jupiter form clouds.
• Different cloud layers
correspond to freezing
points of different
hydrogen compounds.
• Other jovian planets have
similar cloud layers.
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
Jupiter’s
Colors
• Ammonium sulfide clouds (NH4SH) reflect red/brown.
• Ammonia, the highest, coldest layer, reflects white.
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
Saturn’s
Colors
• Saturn’s layers are similar but are deeper in and
farther from the Sun — more subdued.
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
Methane on Uranus and Neptune
• Methane gas on
Neptune and Uranus
absorbs red light but
transmits blue light.
• Blue light reflects
off methane clouds,
making those
planets look blue.
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
Weather on Jovian Planets
• All the jovian planets have strong winds and
storms.
The great red spot on Jupiter
is a storm larger than Earth
that has persisted for centuries.
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
• Big
– massive and cold, they can retain light elements
like hydrogen and helium
Jovian planets are
Temperature
EscapeSpeed
Hydrogen retained
Oxygen retained
Jovian planets
Terrestrial planets
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
Jovian planets are
• Big
– massive and cold, they can retain light elements
like hydrogen and helium
– their composition is like that of the stars
– the smaller terrestrial planets are the abnormal
planets in terms of composition
• Like miniature solar systems
– moons
– rings
Temperature
EscapeSpeed
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
The moons of the Jovian planets
Galilean moons of Jupiter
(“Medici stars”)
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
Sizes of Moons
• Small moons (< 300 km)
— No geological activity
• Medium-sized moons (300–1,500 km)
— Geological activity in past
• Large moons (> 1,500 km)
— Ongoing geological activity
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
Medium and
Large Moons
• Enough self-gravity to
be spherical
• Have substantial
amounts of ice - as
important as rock to
overall composition
• Formed in orbit
around jovian planets
• Circular orbits mostly
in the same direction
as planet rotation
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
Small Moons
• Far more
numerous than
the medium and
large moons
• Not enough
gravity to be
spherical:
“potato-shaped”
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
Some interesting cases:
• Io is the most volcanically active body in the
solar system.
Io
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
Tidal Heating
Io is squished and
stretched as it orbits
Jupiter.
Orbit is elliptical
because of orbital
resonances with
other moons
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
Orbital
Resonances
Every 7 days,
these three
moons line up.
The tugs add up over
time, making all three
orbits elliptical.
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
• Volcanic eruptions continue to change Io’s surface.
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
Europa
• Icy surface
– cracks driven
by some
“geological”
activity
• Liquid ocean
beneath?
– popular spot to
speculate about
the potential
for life
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
Ganymede
• Largest moon in the
solar system
• Clear evidence of
geological activity
• Tidal heating plus
heat from radio-
active decay?
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
Saturn’s large moon Titan
• Titan is the only
moon in the solar
system which has a
thick atmosphere.
• It consists mostly of
nitrogen with some
argon, methane, and
ethane.
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
Titan’s Surface
• The Huygens probe provided a first look at Titan’s surface in
early 2005.
• It had liquid methane, “rocks” made of ice.
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
Neptune’s Moon Triton
• Similar to Pluto, but
larger
• Evidence for past
geological activity
• orbits retrograde
– unique for such a
large moon
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
Saturn’s rings
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
What are Saturn’s rings like?
• They are made up of numerous, small, icy
particles.
• They orbit over Saturn’s equator.
• They are very thin.
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
Artist’s Conception in Ring
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
32
Elaborate structure in rings controlled by the gravity of “shepherd” moons
Pan Prometheus
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
Newly discovered outer ring
33
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
34
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
35
Iapetus
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
actual data
36
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
Jovian Ring Systems
• All four jovian planets have ring systems.
• Others have smaller, darker ring particles than does Saturn.
• Rings and moons ubiquitous around Jovian planets
– like small solar systems.

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Lecture123

  • 1. © 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley The Jovian Planets
  • 2. © 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley The Jovian planets are gas giants - much larger than Earth
  • 3. © 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley Sizes of Jovian Planets • Planets get larger as they get more massive • up to a point... • Planets more massive than Jupiter are expected to shrink. • There comes a point where gravity wins: adding more mass causes contraction.
  • 4. © 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley Jovian Planet Composition • Jupiter and Saturn — Mostly H and He gas — these are the most common elements in the Universe – “Gas Giants” • Uranus and Neptune — Mostly hydrogen compounds: water (H2O), methane (CH4), ammonia (NH3) — Some H, He, and rock — “Ice Giants”
  • 5. © 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley Interiors of Jovian Planets
  • 6. © 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley Inside Jupiter • High pressure inside of Jupiter causes the phase of hydrogen to change with depth. • Hydrogen acts like a metal at great depths because its electrons move freely.
  • 7. © 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley Inside Jupiter • The core is thought to be made of rock, metals, and hydrogen compounds. • The core is about the same size as Earth but 10 times as massive.
  • 8. © 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley Comparing Jovian Interiors • Models suggest that cores of jovian planets have similar composition. • Lower pressures inside Uranus and Neptune mean no metallic hydrogen.
  • 9. © 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley Jupiter’s Atmosphere • Hydrogen compounds in Jupiter form clouds. • Different cloud layers correspond to freezing points of different hydrogen compounds. • Other jovian planets have similar cloud layers.
  • 10. © 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley Jupiter’s Colors • Ammonium sulfide clouds (NH4SH) reflect red/brown. • Ammonia, the highest, coldest layer, reflects white.
  • 11. © 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley Saturn’s Colors • Saturn’s layers are similar but are deeper in and farther from the Sun — more subdued.
  • 12. © 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley Methane on Uranus and Neptune • Methane gas on Neptune and Uranus absorbs red light but transmits blue light. • Blue light reflects off methane clouds, making those planets look blue.
  • 13. © 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley Weather on Jovian Planets • All the jovian planets have strong winds and storms. The great red spot on Jupiter is a storm larger than Earth that has persisted for centuries.
  • 14. © 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley • Big – massive and cold, they can retain light elements like hydrogen and helium Jovian planets are Temperature EscapeSpeed Hydrogen retained Oxygen retained Jovian planets Terrestrial planets
  • 15. © 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley Jovian planets are • Big – massive and cold, they can retain light elements like hydrogen and helium – their composition is like that of the stars – the smaller terrestrial planets are the abnormal planets in terms of composition • Like miniature solar systems – moons – rings Temperature EscapeSpeed
  • 16. © 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley The moons of the Jovian planets Galilean moons of Jupiter (“Medici stars”)
  • 17. © 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley Sizes of Moons • Small moons (< 300 km) — No geological activity • Medium-sized moons (300–1,500 km) — Geological activity in past • Large moons (> 1,500 km) — Ongoing geological activity
  • 18. © 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley Medium and Large Moons • Enough self-gravity to be spherical • Have substantial amounts of ice - as important as rock to overall composition • Formed in orbit around jovian planets • Circular orbits mostly in the same direction as planet rotation
  • 19. © 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley Small Moons • Far more numerous than the medium and large moons • Not enough gravity to be spherical: “potato-shaped”
  • 20. © 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley Some interesting cases: • Io is the most volcanically active body in the solar system. Io
  • 21. © 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley Tidal Heating Io is squished and stretched as it orbits Jupiter. Orbit is elliptical because of orbital resonances with other moons
  • 22. © 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley Orbital Resonances Every 7 days, these three moons line up. The tugs add up over time, making all three orbits elliptical.
  • 23. © 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley • Volcanic eruptions continue to change Io’s surface.
  • 24. © 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley Europa • Icy surface – cracks driven by some “geological” activity • Liquid ocean beneath? – popular spot to speculate about the potential for life
  • 25. © 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley Ganymede • Largest moon in the solar system • Clear evidence of geological activity • Tidal heating plus heat from radio- active decay?
  • 26. © 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley Saturn’s large moon Titan • Titan is the only moon in the solar system which has a thick atmosphere. • It consists mostly of nitrogen with some argon, methane, and ethane.
  • 27. © 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley Titan’s Surface • The Huygens probe provided a first look at Titan’s surface in early 2005. • It had liquid methane, “rocks” made of ice.
  • 28. © 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley Neptune’s Moon Triton • Similar to Pluto, but larger • Evidence for past geological activity • orbits retrograde – unique for such a large moon
  • 29. © 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley Saturn’s rings
  • 30. © 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley What are Saturn’s rings like? • They are made up of numerous, small, icy particles. • They orbit over Saturn’s equator. • They are very thin.
  • 31. © 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley Artist’s Conception in Ring
  • 32. © 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley 32 Elaborate structure in rings controlled by the gravity of “shepherd” moons Pan Prometheus
  • 33. © 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley Newly discovered outer ring 33
  • 34. © 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley 34
  • 35. © 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley 35 Iapetus
  • 36. © 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley actual data 36
  • 37. © 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley Jovian Ring Systems • All four jovian planets have ring systems. • Others have smaller, darker ring particles than does Saturn. • Rings and moons ubiquitous around Jovian planets – like small solar systems.