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The layers
of dense clouds around Jupiter appear in
a photograph of the planet taken by the
Voyager 1 space probe. The large,
oval-shaped mark on the clouds is the
Great Red Spot. The spot is believed to
be an intense atmospheric disturbance.
Image credit: Jet Propulsion Laboratory |
Jupiter is the largest
planet in the solar system. Its diameter is
88,846 miles (142,984 kilometers), more than 11
times that of Earth, and about one-tenth that of
the sun. It would take more than 1,000 Earths to
fill up the volume of the giant planet. When
viewed from Earth, Jupiter appears brighter than
most stars. It is usually the second brightest
planet -- after Venus.
Jupiter is the fifth
planet from the sun. Its mean (average) distance
from the sun is about 483,780,000 miles
(778,570,000 kilometers), more than five times
Earth's distance. Ancient astronomers named
Jupiter after the king of the Roman gods.
Astronomers have
studied Jupiter with telescopes based on Earth
and aboard artificial satellites in orbit around
Earth. In addition, the United States has sent
six space probes (crewless exploratory craft) to
Jupiter.
Astronomers witnessed a
spectacular event in July 1994, when 21
fragments of a comet named Shoemaker-Levy 9
crashed into Jupiter's atmosphere. The impacts
caused tremendous explosions, some scattering
debris over areas larger than the diameter of
Earth.
Physical features of
Jupiter
Jupiter is a giant ball
of gas and liquid with little, if any, solid
surface. Instead, the planet's surface is
composed of dense red, brown, yellow, and white
clouds. The clouds are arranged in light-colored
areas called zones and darker regions called
belts that circle the planet parallel to the
equator.
Orbit and rotation
Jupiter travels around
the sun in a slightly elliptical (oval-shaped)
orbit. The planet completes one orbit in 4,333
Earth days, or almost 12 Earth years.
As Jupiter orbits the
sun, the planet rotates on its axis, an
imaginary line through its center. The axis is
tilted about 3¡. Scientists measure tilt
relative to a line at a right angle to the
orbital plane, an imaginary surface touching all
points of the orbit.
Jupiter rotates faster
than any other planet. It takes 9 hours 56
minutes to spin around once on its axis,
compared with 24 hours for Earth. Scientists
cannot measure the rotation of the interior of
the giant planet directly, so they have
calculated the speed from indirect measurements.
They first calculated the speed using an average
of the speeds of the visible clouds that move
with interior currents, except for a more rapid
zone near the equator.
Jupiter sends out radio
waves strong enough to be picked up by radio
telescopes on Earth. Scientists now measure
these waves to calculate Jupiter's rotational
speed. The strength of the waves varies under
the influence of Jupiter's magnetic field in a
pattern that repeats every 9 hours 56 minutes.
Because the magnetic field originates in
Jupiter's core, this variation shows how fast
the plant's interior spins.
Jupiter's rapid
rotation makes it bulge at the equator and
flatten at the poles. The planet's diameter is
about 7 percent larger at the equator than at
the poles.
Mass and density
Jupiter is heavier than
any other planet. Its mass (quantity of matter)
is 318 times larger than that of Earth. Although
Jupiter has a large mass, it has a relatively
low density. Its density averages 1.33 grams per
cubic centimeter, slightly more than the density
of water. The density of Jupiter is about 1/4
that of Earth. Because of Jupiter's low density,
astronomers believe that the planet consists
primarily of hydrogen and helium, the lightest
elements. Earth, on the other hand, is made up
chiefly of metals and rock. Jupiter's mix of
chemical elements resembles that of the sun,
rather than that of Earth.
Jupiter may have a core
made up of heavy elements. The core may be of
about the same chemical composition as Earth,
but 20 or 30 times more massive.
The force of gravity at
the surface of Jupiter is up to 2.4 times
stronger than on Earth. Thus, an object that
weighs 100 pounds on Earth would weigh as much
as 240 pounds on Jupiter.
The atmosphere of
Jupiter is composed of about 86 percent
hydrogen, 14 percent helium, and tiny amounts of
methane, ammonia, phosphine, water, acetylene,
ethane, germanium, and carbon monoxide. The
percentage of hydrogen is based on the number of
hydrogen molecules in the atmosphere, rather
than on their total mass. Scientists have
calculated these amounts from measurements taken
with telescopes and other instruments on Earth
and aboard spacecraft.
These chemicals have
formed colorful layers of clouds at different
heights. The highest white clouds in the zones
are made of crystals of frozen ammonia. Darker,
lower clouds of other chemicals occur in the
belts. At the lowest levels that can be seen,
there are blue clouds. Astronomers had expected
to detect water clouds about 44 miles (70
kilometers) below the ammonia clouds. However,
none have been discovered at any level.
Jupiter's most outstanding
surface feature is the Great Red Spot, a
swirling mass of gas resembling a hurricane. The
widest diameter of the spot is about three times
that of Earth. The color of the spot usually
varies from brick-red to slightly brown. Rarely,
the spot fades entirely. Its color may be due to
small amounts of sulfur and phosphorus in the
ammonia crystals.
The edge of the Great
Red Spot circulates at a speed of about 225
miles (360 kilometers) per hour. The spot
remains at the same distance from the equator
but drifts slowly east and west.
The zones, belts, and
the Great Red Spot are much more stable than
similar circulation systems on Earth. Since
astronomers began to use telescopes to observe
these features in the late 1600's, the features
have changed size and brightness but have kept
the same patterns.
Temperature
The temperature at the
top of Jupiter's clouds is about -230 degrees F
(-145 degrees C). Measurements made by ground
instruments and spacecraft show that Jupiter's
temperature increases with depth below the
clouds. The temperature reaches 70 degrees F (21
degrees C) -- "room temperature" -- at a level
where the atmospheric pressure is about 10 times
as great as it is on Earth. Scientists speculate
that if Jupiter has any form of life, the life
form would reside at this level. Such life would
need to be airborne, because there is no solid
surface at this location on Jupiter. Scientists
have discovered no evidence for life on Jupiter.
Near the planet's
center, the temperature is much higher. The core
temperature may be about 43,000 degrees F
(24,000 degrees C) -- hotter than the surface of
the sun.
Jupiter is still losing
the heat produced when it became a planet. Most
astronomers believe that the sun, the planets,
and all the other bodies in the solar system
formed from a spinning cloud of gas and dust.
The gravitation of the gas and dust particles
packed them together into dense clouds and solid
chunks of material. By about 4.6 billion years
ago, the material had squeezed together to form
the various bodies in the solar system. The
compression of material produced heat. So much
heat was produced when Jupiter formed that the
planet still radiates about twice as much heat
into space as it receives from sunlight.
Magnetic field
Like Earth and many
other planets, Jupiter acts like a giant magnet.
The force of its magnetism extends far into
space in a region surrounding the planet called
its magnetic field. Jupiter's magnetic field is
about 14 times as strong as Earth's, according
to measurements made by spacecraft. Jupiter's
magnetic field is the strongest in the solar
system, except for fields associated with
sunspots and other small regions on the sun's
surface.
Scientists do not fully
understand how planets produce magnetic fields.
They suspect, however, that the movement of
electrically charged particles in the interior
of planets generates the fields. Jupiter's field
would be so much stronger than Earth's because
of Jupiter's greater size and faster rotation.
Jupiter's magnetic
field traps electrons, protons, and other
electrically charged particles in radiation
belts around the planet. The particles are so
powerful that they can damage instruments aboard
spacecraft operating near the planet.
Within a region of
space called the magnetosphere, Jupiter's
magnetic field acts as a shield. The field
protects the planet from the solar wind, a
continuous flow of charged particles from the
sun. Most of these particles are electrons and
protons traveling at a speed of about 310 miles
(500 kilometers) per second. The field traps the
charged particles in the radiation belts. The
trapped particles enter the magnetosphere near
the poles of the magnetic field. On the side of
the planet away from the sun, the magnetosphere
stretches out into an enormous magnetic tail,
often called a magnetotail, that is at least 435
million miles (700 million kilometers) long.
Radio waves given off
by Jupiter reach radio telescopes on Earth in
two forms -- bursts of radio energy and
continuous radiation. Strong bursts occur when
Io, the closest of Jupiter's four large moons,
passes through certain regions in the planet's
magnetic field. Continuous radiation comes from
Jupiter's surface as well as from high-energy
particles in the radiation belts.
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Callisto,
a moon of Jupiter, is covered with
craters produced when asteroids and
comets struck its icy surface. Beneath
the surface may be an ocean of salty
liquid water. Image credit: NASA |
Satellites
Jupiter has 16
satellites that measure at least 6 miles (10
kilometers) in diameter. It also has many
smaller satellites. Jupiter's four largest
satellites, in order of their distance from
Jupiter, are Io, Europa, Ganymede, and Callisto.
These four moons are called the Galilean
satellites. The Italian astronomer Galileo
discovered them in 1610 with one of the earliest
telescopes.
Io has many active
volcanoes, which produce gases containing
sulfur. The yellow-orange surface of Io probably
consists largely of solid sulfur that was
deposited by the eruptions. Europa ranks as the
smallest of the Galilean satellites, with a
diameter of 1,945 miles (3,130 kilometers).
Europa has a smooth, cracked, icy surface.
The largest Galilean
satellite is Ganymede, with a diameter of 3,273
miles (5,268 kilometers). Ganymede is larger
than the planet Mercury. Callisto, with a
diameter of 2,986 miles (4,806 kilometers), is
slightly smaller than Mercury. Ganymede and
Callisto appear to consist of ice and some rocky
material. The two satellites have many craters.
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Ganymede,
a moon of Jupiter, has craters and
cracks on its surface. Asteroids and
comets that hit Ganymede made the
craters. The cracks are due to expansion
and contraction of the surface. Image
credit: NASA |
Jupiter's remaining
satellites are much smaller than the Galilean
moons. Amalthea and Himalia are the next
largest. Potato-shaped Amalthea is about 163
miles (262 kilometers) in its long dimension.
Himalia is 106 miles (170 kilometers) in
diameter. Most of the remaining satellites were
discovered by astronomers using large telescopes
on Earth. Scientists discovered Metis and
Adrastea in 1979 by studying pictures that had
been taken by the Voyager spacecraft.
Rings
Jupiter has three thin
rings around its equator. They are much fainter
than the rings of Saturn. Jupiter's rings appear
to consist mostly of fine dust particles. The
main ring is about 20 miles (30 kilometers)
thick and more than 4,000 miles (6,400
kilometers) wide. It circles the planet inside
the orbit of Amalthea.
The impact of Comet
Shoemaker-Levy 9
In March 1993,
astronomers Eugene Shoemaker, Carolyn Shoemaker,
and David H. Levy discovered a comet near
Jupiter. The comet, later named Shoemaker-Levy
9, probably once orbited the sun independently,
but had been pulled by Jupiter's gravity into an
orbit around the planet. When the comet was
discovered, it had broken into 21 pieces. The
comet probably had broken apart when it passed
close to Jupiter.
Calculations based on
the comet's location and velocity showed that
the fragments would crash into Jupiter's
atmosphere in July 1994. Scientists hoped to
learn much about the effects of a collision
between a planet and a comet.
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Scars from
the crash of Comet Shoemaker-Levy 9
appear on Jupiter's surface as a series
of maroon blotches in this photo. The
comet broke into 21 pieces before it hit
Jupiter in 1994. Image credit: Hubble
Space Telescope Comet Team and NASA |
Astronomers at all the
major telescopes on Earth turned their
instruments toward Jupiter at the predicted
collision times. Scientists also observed
Jupiter with the powerful Hubble Space
Telescope, which is in orbit around Earth; and
the remotely controlled space probe Galileo,
which was on its way to Jupiter.
The fragments fell on
the back side of Jupiter as viewed from Earth
and the Hubble Space Telescope. But the rotation
of Jupiter carried the impact sites around to
the visible side after less than half an hour.
Scientists estimate that the largest fragments
were about 0.3 to 2.5 miles (0.5 to 4
kilometers) in diameter. The impacts were
directly observable from Galileo, which was
within about 150 million miles (240 million
kilometers) from Jupiter. However, damage to
certain of the probe's instruments limited its
ability to record and send data.
The impacts caused
large explosions, probably due to the
compression, heating, and rapid expansion of
atmospheric gases. The explosions scattered
comet debris over large areas, some with
diameters larger than that of Earth. The debris
gradually spread into a dark haze of fine
material that remained suspended for several
months in Jupiter's upper atmosphere. If a
similar comet ever collided with Earth, it might
produce a haze that would cool the atmosphere
and darken the planet by absorbing sunlight. If
the haze lasted long enough, much of Earth's
plant life could die, along with the people and
animals that depend on plants.
Flights to Jupiter
The United States has
sent six space probes to Jupiter: (1) Pioneer
10, (2) Pioneer-Saturn, (3) Voyager 1, (4)
Voyager 2, (5) Ulysses, and (6) Galileo.
Pioneer 10 was launched
in 1972 and flew within 81,000 miles (130,000
kilometers) of Jupiter on Dec. 3, 1973. The
probe revealed the severe effects of Jupiter's
radiation belt on spacecraft. Pioneer 10 also
reported the amount of hydrogen and helium in
the planet's atmosphere. In addition, the probe
discovered that Jupiter has an enormous
magnetosphere.
Pioneer-Saturn flew
within 27,000 miles (43,000 kilometers) of
Jupiter in December 1974. The craft provided
close-up photographs of Jupiter's polar regions
and data on the Great Red Spot, the magnetic
field, and atmospheric temperatures.
Voyager 1 and Voyager 2
flew past Jupiter in March and July 1979,
respectively. These craft carried more sensitive
instruments than did the Pioneers, and
transmitted much more information. Astronomers
used photographs taken by the Voyagers to make
the first detailed maps of the Galilean
satellites. The Voyagers also revealed sulfur
volcanoes on Io, discovered lightning in
Jupiter's clouds, and mapped flow patterns in
the cloud bands.
Ulysses was launched in
October 1990 and passed by Jupiter in February
1992. The European Space Agency, an organization
of Western European nations, had built the probe
mainly to study the sun's polar regions.
Scientists used the tremendous gravitational
force of Jupiter to put Ulysses into an orbit
that would take it over the sun's polar regions.
As Ulysses passed by Jupiter, it gathered data
indicating that the solar wind has a much
greater effect on Jupiter's magnetosphere than
earlier measurements had suggested.
Galileo began its
journey to Jupiter in October 1989. The craft
released an atmospheric probe in July 1995. In
December 1995, the probe plunged into Jupiter's
atmosphere. The probe penetrated deep into the
cloud layers and measured the amount of water
and other chemicals in the atmosphere. Also in
December 1995, Galileo went into orbit around
Jupiter. Over the next several years, the craft
monitored Jupiter's atmosphere and observed the
planet's major satellites. Galileo's mission was
extended in 1997 and again in 1999. Eventually,
however, the craft ran low on fuel. In September
2003, mission managers intentionally crashed
Galileo into Jupiter's atmosphere to avoid any
risk of the craft crashing into and
contaminating Jupiter's moon Europa. Galileo's
observations of Europa had shown that it might
have an ocean below its surface capable of
supporting life.
Contributors:
Peter J. Gierasch, Ph.D., Professor of
Astronomy, Cornell University. Philip D.
Nicholson, Ph.D., Professor of Astronomy,
Cornell University.