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Transcript
The Jovian Planets
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© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
Great Exam Performance!
• Class average was 79.5%
• This is the highest average I’ve ever had on
any ASTR 100 exam
Wonderful job!
• Exams will be handed back in your sections
• Don’t let up; next exam has more concepts
and is likely to be tougher
2
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
The Jovian planets are
gas giants much larger than Earth
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© 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
• Uranus and Neptune
— Mostly hydrogen compounds: water (H2O),
methane (CH4), ammonia (NH3)
— Some H, He, and rock
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© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
Interiors of Jovian Planets
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© 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.
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© 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.
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© 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.
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© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
• Big
Jovian planets are
– massive and cold, they can retain light elements
like hydrogen and helium
Jovian planets
ed
n
i
a
ret
Escape Speed
en
g
o
r
Hyd
s
t
e
n
la
p
l
a
ed
i
r
n
t
i
s
a
t
e
Terr ygen re
Ox
Temperature
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
– moons
– rings
Escape Speed
• Like miniature solar systems
16
Temperature
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
Big Moons of Jupiter
Jupiter’s inner big moon, Io, is smaller than Mercury
but has active volcanos. What could supply the energy?
A.Tidal squeezing by Jupiter
B. Radiation from Jupiter
C. Heat from the formation of Io
D. Radioactive elements inside Io
E. I don’t know
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The moons of the Jovian planets
Galilean moons of Jupiter
(“Medici stars”)
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© 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
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© 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 rotation20
© 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”
21
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
Some interesting cases:
Io
• Io is the most volcanically active body in the
solar system.
22
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
Tidal Heating
Io is squished and
stretched as it orbits
Jupiter.
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
Orbit is elliptical
because of orbital
resonances with
23
other moons
Orbital
Resonances
The tugs add up over
time, making all three
orbits elliptical.
Every 7 days,
these three
moons line up.
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© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
25
• 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
26
© 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 radioactive decay?
27
© 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.
28
© 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.
29
© 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
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© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
Saturn’s rings
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© 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.
32
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
Artist’s Conception of Ring
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© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
Elaborate structure in rings controlled by the gravity of “shepherd” moons
Pan
Prometheus
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© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
Newly discovered outer ring
Co-discovered by our own Professor Doug Hamilton!
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© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
Iapetus
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© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley
actual data
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© 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.
39
© 2007 Pearson Education Inc., publishing as Pearson Addison-Wesley