JUPITER: KING OF THE PLANETS
JUPITER IS EASILY THE PLANETARY CHAMPION:
Mass is 318 times that of Earth = 1.9 x 10^30 g
Radius is 71,492 km or 11.21 times Earth's.
Density is only 1.33 g/cm^3 or 0.241 of Earth's.
As seen from Earth:
Third brightest object in the night sky.
Period of 11.86 years.
Semi-major axis of 5.20 AU, e = 0.048.
13 moons discovered from the ground.
No solid surface: differential rotation
Magnetic (interior) spin period: 9h 55m
So fast that ellipticity is over 6.5%
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JUPITER'S ATMOSPHERE
Composition
Primordial as v_esc = 59.5 km/s
86% H_2 by number; 14% He
Small amounts of: CH_4, NH_3, H_2O
Key Features
BRIGHT ZONES and DARK BELTS
Produced by convection currents:
Zones are higher pressure: rising warm
Belts are lower pressure: sinking cool
Very fast rotation spreads these out E/W
Winds up to 400 km/h
SPOTS and OVALS -- GIANT STORMS
Great Red Spot: lasted over 300 years but varies
in size
-- a persistent storm w/ counterclockwise flow
White Ovals: over 40 years -- high regions
Brown Ovals: holes in clouds -- see depths
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Vertical Structure of Atmosphere
NO SOLID SURFACE: Min T (110K) at top of
troposphere defines 0 km level
There P approx 0.1 P_{oplus}
Wien's Law: T = 125K <-- immense internal heat
of formation still leaking out
Below this, cloud layers:
Ammonia ice (white)
Ammonium hydrosulfide (NH_4SH) ice (yellow/brown) --
colorations from Sulfur and S compounds
Water ice (white/blue)
Galileo ``lander'' probed atmosphere in 1995
penetrated to -150 km
400 K, P approx 30 P_Earth
Deep strong winds --> internal heating
Ethane (C_2H_6) and phosphine (PH_3) found
(some coloring)
but no organic molecules.
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JUPITER'S INTERIOR
All numbers are approximate: from the best theoretical models,
but no direct data, of course.
Clouds probably end at -400 km
MOLECULAR HYDROGEN GAS:
20,000 km thick layer
P rises to 3,000,000 atm
T increases to 11,000~K
LIQUID METALLIC HYDROGEN:
40,000 km thick layer
P rises to 12,000,000 atm
T rises to 25,000 K
ROCKY/METALLIC CORE:
Roughly 10,000 km in radius
Central P about 50,000,000 atm
Central T about 40,000 K
Crushed to about 25 g/cm^3 at center
captured asteroid(s); known from Earth
4 more captured moons around 23,000,000 km out: these
have retrograde orbits.
Many more small moons have been discovered recently by the
Galileo spacecraft, for a total of 61 known in 2003
-- all small;
most presumably captured asteroids.
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DETAILS ON THE GALILEAN MOONS
IO: most active object in SS
a = 422,000 km; D = 3640 km; M = 1.22 M_{Moon}
A multicolored surface: yellow, orange, red, brown, and white.
Thick rocky mantle; Fe/FeS core: rho = 3.5 g/cm^3
Powerful tidal flexures: P = 1.77d = 1/2 P(Europa)
~= 1/4 P(Ganymede) --> forced heating
Sulfur volcanos blasting out particles
Very smooth, young ( < 1 Myr) surface: new flows
Fills up Jupiter's plasma torus with ionized S atoms.
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EUROPA: Icy & Oceanic?
a = 671,000 km
D = 3130 km
M = 0.65 M_{Moon}
rho = 3.04 g/cm^3
Icy crust kms thick, temporary cracks
Colored areas mostly mineral rich ices
Probable 100 km thick ocean -- LIFE EXISTS(ED) THERE ????
Surface < 100 Myr old with new ice replacing old
Less heating by tidal flexure than Io, but still a good bit
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GANYMEDE: King of the Moons
a = 1,070,000 km
D = 5270 km
M = 2.02 M_{Moon}
rho = 1.93 g/cm^3 -- > very thick ice layer
Rocky mantle, Fe/FeS core
Many craters, many old ones survive
Grooved terrain -- > plate tectonics at 3 Gy
Only satellite with a magnetic field