Photo: http://photojournal.jpl.nasa.gov/

 

Jupiter

Jupiter was the roman version of the Greek god Zeus. King of the Olympus gods and son of Chronos.

The most massive planet in our solar system, with four planet-sized moons and many smaller moons, Jupiter forms a kind of miniature solar system. Jupiter resembles a star in composition. In fact, if it had been about eighty times more massive, it would have become a star rather than a planet.

On January 7, 1610, using his primitive telescope, astronomer Galileo Galilei saw four small 'stars' near Jupiter. He had discovered Jupiter's four largest moons, now called Io, Europa, Ganymede, and Callisto. Collectively, these four moons are known today as the Galilean satellites.

Galileo would be astonished at what we have learned about Jupiter and its moons in the past 30 years. Io is the most volcanically active body in our solar system. Ganymede is the largest planetary moon and is the only moon in the solar system known to have its own magnetic field. A liquid ocean may lie beneath the frozen crust of Europa. Icy oceans may also lie deep beneath the crusts of Callisto and Ganymede. In 2003 alone, astronomers discovered 23 new moons orbiting the giant planet, giving Jupiter a total moon count of 63 - the most in the solar system. The numerous small outer moons may be asteroids captured by the giant planet's gravity.

Jupiter's appearance is a tapestry of beautiful colors and atmospheric features. Most visible clouds are composed of ammonia. Water exists deep below and can sometimes be seen through clear spots in the clouds. The planet's 'stripes' are dark belts and light zones created by strong east-west winds in Jupiter's upper atmosphere. Within these belts and zones are storm systems that have raged for years. The Great Red Spot, a giant spinning storm, has been observed for more than 300 years.

The composition of Jupiter's atmosphere is similar to that of the Sun - mostly hydrogen and helium. Deep in the atmosphere, the pressure and temperature increase, compressing the hydrogen gas into a liquid. At depths about a third of the way down, the hydrogen becomes metallic and electrically conducting. In this metallic layer, Jupiter's powerful magnetic field is generated by electrical currents driven by Jupiter's fast rotation. At the center, the immense pressure may support a solid core of ice-rock about the size of Earth.

Jupiter's enormous magnetic field is nearly 20,000 times as powerful as Earth's. Trapped within Jupiter's magnetosphere (the area in which magnetic field lines encircle the planet from pole to pole) are swarms of charged particles. Jupiter's rings and moons are embedded in an intense radiation belt of electrons and ions trapped in the magnetic field. The jovian magnetosphere, comprising these particles and fields, balloons 1 to 3 million kilometers (600,000 to 2 million miles) toward the Sun and tapers into a windsock-shaped tail extending more than 1 billion kilometers (600 million miles) behind Jupiter as far as Saturn's orbit.

Discovered in 1979 by NASA's Voyager 1 spacecraft, Jupiter's rings were a surprise: a flattened main ring and an inner cloud-like ring, called the halo, are both composed of small, dark particles. A third ring, known as the gossamer ring because of its transparency, is actually three rings of microscopic debris from three small moons: Amalthea, Thebe, and Adrastea. Jupiter's ring system may be formed by dust kicked up as interplanetary meteoroids smash into the giant planet's four small inner moons. The main ring probably comes from the moon Metis. Jupiter's rings are only visible when backlit by the Sun.

In December 1995, NASA's Galileo spacecraft dropped a probe into Jupiter's atmosphere, which collected the first direct measurements of Jupiter's atmosphere. Following the release of the probe, the Galileo spacecraft began a multiyear study of Jupiter and the largest moons. As Galileo began its 29th orbit, the Cassini-Huygens spacecraft was nearing Jupiter for a gravity-assist maneuver on the way to Saturn. The two spacecraft made simultaneous observations of the magnetosphere, solar wind, rings, and Jupiter's auroras.

 

Jupiter facts  
Distance from Sun 778.3 million km
Equatorial diameter 142,984 km (88,864 mi.)
Equatorial diameter (Earth=1) 11.209
Mass (Earth=1) 317.9
Mean density 1.3 g/cm³
Axial period 9.8 hours
Axial inclination 3.1°
Orbital period 11.86 years
Orbital inclination 1.3°
Orbital eccentricity 0.048
Gravity at cloud-tops (Earth=1) 2.64
Escape velocity 60.2 km/s (216,720 km/hr, 134,692 mi./hr)
Atmospheric composition ~90% hydrogen, ~10% helium, traces of methane, etc
Mean temperature (cloud tops) -150°C (-238°F)
Albedo 0.43
Number of moons 69

 

Jupiter moons

1 Io  24 Iocaste  47 Eukelade 
2 Europa  25 Erinome  48 Cyllene 
3 Ganymede  26 Isonoe  49 Kore 
4 Callisto  27 Praxidike  50 Herse 
5 Amalthea  28 Autonoe  Provisional names
6 Himalia  29 Thyone  1 S/2000 J11 
7 Elara  30 Hermippe  2 S/2003 J2 
8 Pasiphae  31 Aitne  3 S/2003 J3 
9 Sinope  32 Eurydome  4 S/2003 J4 
10 Lysithea  33 Euanthe  5 S/2003 J5 
11 Carme  34 Euporie  6 S/2003 J9 
12 Ananke  35 Orthosie  7 S/2003 J10 
13 Leda  36 Sponde  8 S/2003 J12 
14 Thebe  37 Kale  9 S/2003 J15 
15 Adrastea  38 Pasithee  10 S/2003 J16 
16 Metis  39 Hegemone  11 S/2003 J18 
17 Callirrhoe  40 Mneme  12 S/2003 J19 
18 Themisto  41 Aoede  13 S/2003 J23 
19 Megaclite  42 Thelxinoe  14 S/2010 J 1 
20 Taygete  43 Arche  15 S/2010 J 2 
21 Chaldene  44 Kallichore  16 S/2011 J1 
22 Harpalyke  45 Helike  17 S/2011 J2
23 Kalyke  46 Carpo 

 

Jupiter Rings
Ring Distance Width Mass
  (km) (km) (kg)
Halo 100,000 22,800 ?
Main 122,800 6,400 1.00E+13
Gossamer interior 129,200 52,200 ?
Gossamer exterior 182,000 42,900 ?

Information from SSE-JPL-NASA - Wikipedia

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