A few scientific facts about Jupiter

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Transcript A few scientific facts about Jupiter

Jupiter
Jupiter (Iuppiter, Juppiter) or Jove, King of the
Roman gods (fifth planet from the sun).
He gave day and night to mankind, sent the
snow and the rain, and caused the winds to
blow and the dark storm clouds to gather
A few scientific facts about Jupiter:
Master of its orbit, the fifth planet holds a faint ring system and at least
sixteen moons in its gravitational grip
Four moons are as big as small planets
The combined pulls of Jupiter and the Sun also keep two asteroid groups,
called the Trojans, in Jupiter’s orbit.
One group moves along a sixth of the way ahead of Jupiter, the other
equally far behind.
They bear heroes’ names from the ancient Trojan War; the first group
represents Greece, the second Troy.
As heavyweight champion of the worlds, Jupiter accounts for more than
two-thirds of all material in the Solar System outside the Sun.
Gravity two and a half times stronger than our own creates intense
pressures in the swirling gases of its atmosphere.
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 Earthyears.
The axis is tilted about 3 degrees
Jupiter rotates
faster than any
other planet. It
takes 9 hours 55
minutes to spin
around once on its
axis
Figure 11.2 Rotational Flattening All spinning objects tend to develop an
equatorial bulge because rotation causes matter to push outward against the
inward-pulling gravity. The size of the bulge depends on the mechanical
strength of the matter and the rate of rotation. The inward-pointing arrows
denote gravity, the outward arrows the “push” due to rotation
Mass and density
Jupiter is heavier than any other planet.
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.
Jupiter's mix of chemical elements resembles that of the sun, rather than that
of Earth.
The force of gravity at the
surface of Jupiter is up to 2.4
times stronger than on Earth.
Magnetic field
Jupiter's magnetic field is about 14 times as strong as Earth's
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 suspect, however, that the movement of electrically
charged particles in the interior of planets generates the fields
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.
Rings
Jupiter has thin rings,
discovered in 1979 when the
Voyager spacecraft passed
by the planet, 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.
In 1998, scientists at Cornell
University in Ithaca, New York,
and the National Optical
Astronomy Observatories in
Tucson, Arizona, announced that
they had determined the origin of
Jupiter's rings by analyzing data
from NASA's Galileo spacecraft,
orbiting the planet since 1995.
Voyager images showed only three
rings around Jupiter--a thin main
ring, a broader inner ring called
the halo, and a transparent outer
ring called the gossamer ring. The
new images from Galileo revealed
that Jupiter's gossamer ring is
actually two rings, one embedded
in the other.
The pictures also revealed that
dust from two of Jupiter's smaller
moons, Amalthea and Thebe, which
orbit near the gossamer ring, is
the same kind of dust that is found
in the rings. Scientists decided
that the dust is pulverized
material from the two moons,
kicked off the surface by the
impact of meteoroids. The larger
main ring of Jupiter is probably
formed by dust produced by
meteoroid collisions with other
Jovian moons.
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.
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.
A region near Jupiter's
equator appears yellowish
to the naked eye (top). An
infrared camera, however,
reveals a dark blue spot
(bottom, center) that
indicates a warm region
deep below the high, cold
clouds of Jupiter's
atmosphere.
NASA
Atmosphere
86% Hydrogen, 14% helium, methane, ammonia, carbon
monoxide, ethane, acetylene, phosphine, water vapor.
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.
The bands of dark and light clouds on Jupiter are a distinctive
feature of its atmosphere. In fact, they represent regions of varying
pressure; the light bands are high-pressure 'zones', and the dark
bands are low-pressure 'belts'.
Figure 11.5 Zonal
Flow The wind speed
in Jupiter’s
atmosphere,
measured relative to
the planet’s internal
rotation rate.
Alternations in wind
direction are
associated with the
atmospheric band
structure.
The equatorial regions of the atmosphere rotate faster than
the planet, with an average flow speed of some 85 m/s, or
about 300 km/h, in the easterly direction. The speed of this
equatorial flow is quite similar to that of the jet stream on
Earth
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