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THE JOVIAN PLANETS 
Giants of the Solar System 
Observations of Jupiter and Saturn 
The Discoveries of Uranus and Neptune 
The Jovian Planets In Bulk 
Jupiter’s Atmosphere 
The Atmosphere of the Outer Jovian Worlds 
•Interior Structure 
•Internal Heating 
Jovian Magnetosphere 
Interlude-A Planetary Impact
THE JOVIAN PLANETS
Jovian planets are also known as gas giants. There are four Jovian planets: Jupiter, Saturn, 
Uranus, and Neptune. These four planets also comprise the outer planets. The term Jovian came 
from Jupiter, describing the other gas giants in our Solar System as Jupiter-like. Despite 
common belief, gas giants are not composed entirely of gas. A rocky core exists somewhere 
within these balls of gas, but it is difficult if not impossible as of yet, to determine where this 
center is. Because of the intense high temperatures in the middle of these planets, the rocky core 
of a gas giant is actually believed to be liquid heavy compounds, such as nickel. Thus, it is 
sometimes misleading when astronomers refer to the rocky core of these planets. The Jovian 
planets are larger than the other planets of the Solar System and have dozens of moons.
THE DISCOVERIES OF URANUS AND NEPTUNE 
• The five planets visible with the unaided eye are Mercury, Venus, Mars, Jupiter 
and Saturn. If you know where to look, you can’t miss them, even in light 
polluted skies. But there are two planets, Uranus and Neptune, which are a 
little harder to find. You’ll need a telescope to even see them. 
• Both Uranus and Neptune were discovered after the invention of the telescope. 
Galileo first pointed his crude telescope at the heavens, but other astronomers 
actually discovered Uranus and Neptune. Uranus was found in 1781 by 
William Herschel, and Neptune was found in 1846 based on calculations by 
John Couch Adams in England and Urbain Le Leverrier in France.
THE JOVIAN PLANETS IN BULK 
• Most of the masses of Jupiter and Saturn, and about half those of Uranus and 
Neptune, are made up of hydrogen and helium—light gases on Earth (having 
densities 0.08 and 0.16 kg/m3, respectively, at room temperature and sea level), 
but compressed enormously by these planets’ strong gravitational fields. The 
abundance of hydrogen and helium on these worlds is itself a consequence of the 
strong Jovian gravity. The Jovian planets are massive enough to have retained even 
the lightest gas, hydrogen, and very little of their original atmospheres have 
escaped since the birth of the solar system 4.6 billion years ago. At the heart of 
each Jovian planet lies a dense, compact core many times more massive than 
Earth. 
• None of the Jovian planets has a solid surface of any kind. Their gaseous 
atmospheres just become denser with depth because of the pressure of the 
overlying layers, eventually becoming liquid in the interior. The surface we see 
from Earth is simply the top of the outermost layer of atmospheric clouds.
JUPITER’S ATMOSPHERE 
• The atmosphere of Jupiter is the largest planetary atmosphere in the Solar System. It is 
mostly made of molecular hydrogen and helium in roughly solar proportions; other 
chemical compounds are present only in small amounts and include methane, ammonia, 
hydrogen sulfide and water. Although water is thought to reside deep in the atmosphere, 
its directly measured concentration is very low. The oxygen, nitrogen, sulfur, and noble 
gas abundances in Jupiter's atmosphere exceed solar values by a factor of about three. 
• The Jovian atmosphere shows a wide range of active phenomena, including band 
instabilities, vortices (cyclones and anticyclones), storms and lightning.The vortices reveal 
themselves as large red, white or brown spots (ovals). The largest two spots are the Great 
Red Spot(GRS) and Oval BA which is also red. These two and most of the other large spots 
are anticyclonic. Smaller anticyclones tend to be white. Vortices are thought to be relatively 
shallow structures with depths not exceeding several hundred kilometers. Located in the 
southern hemisphere, the GRS is the largest known vortex in the Solar System. It could 
engulf several Earths and has existed for at least three hundred years. Oval BA, south of 
GRS, is a red spot a third the size of GRS that formed in 2000 from the merging of three 
white ovals.
THE ATMOSPHERE OF THE OUTER JOVIAN WORLDS 
• The atmospheres of Jupiter and Saturn are made almost entirely of hydrogen and helium, 
although there is some evidence they contain hydrogen compounds. Uranus and Neptune are 
made primarily of hydrogen compounds, with smaller traces of hydrogen, helium, metal and 
rock. The most common hydrogen compounds are methane (CH4), ammonia (NH3), and water 
(H2O). 
• The farther away a planet is from the Sun, the cooler its atmosphere will be. This means that 
the same gases will condense to form clouds at different altitudes on different planets because 
the condensation of a gas requires a specific amount of pressure and temperature. Ammonia, 
ammonium hydrosulfide and water make up the 3 cloud layers of Jupiter and Saturn. You can 
see from the graph to the right that these condense at lower altitudes in Saturn's atmosphere 
than they do in Jupiter's atmosphere.

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JOVIAN PLANETS BY KYLE YVONNE

  • 1. THE JOVIAN PLANETS Giants of the Solar System Observations of Jupiter and Saturn The Discoveries of Uranus and Neptune The Jovian Planets In Bulk Jupiter’s Atmosphere The Atmosphere of the Outer Jovian Worlds •Interior Structure •Internal Heating Jovian Magnetosphere Interlude-A Planetary Impact
  • 3. Jovian planets are also known as gas giants. There are four Jovian planets: Jupiter, Saturn, Uranus, and Neptune. These four planets also comprise the outer planets. The term Jovian came from Jupiter, describing the other gas giants in our Solar System as Jupiter-like. Despite common belief, gas giants are not composed entirely of gas. A rocky core exists somewhere within these balls of gas, but it is difficult if not impossible as of yet, to determine where this center is. Because of the intense high temperatures in the middle of these planets, the rocky core of a gas giant is actually believed to be liquid heavy compounds, such as nickel. Thus, it is sometimes misleading when astronomers refer to the rocky core of these planets. The Jovian planets are larger than the other planets of the Solar System and have dozens of moons.
  • 4. THE DISCOVERIES OF URANUS AND NEPTUNE • The five planets visible with the unaided eye are Mercury, Venus, Mars, Jupiter and Saturn. If you know where to look, you can’t miss them, even in light polluted skies. But there are two planets, Uranus and Neptune, which are a little harder to find. You’ll need a telescope to even see them. • Both Uranus and Neptune were discovered after the invention of the telescope. Galileo first pointed his crude telescope at the heavens, but other astronomers actually discovered Uranus and Neptune. Uranus was found in 1781 by William Herschel, and Neptune was found in 1846 based on calculations by John Couch Adams in England and Urbain Le Leverrier in France.
  • 5. THE JOVIAN PLANETS IN BULK • Most of the masses of Jupiter and Saturn, and about half those of Uranus and Neptune, are made up of hydrogen and helium—light gases on Earth (having densities 0.08 and 0.16 kg/m3, respectively, at room temperature and sea level), but compressed enormously by these planets’ strong gravitational fields. The abundance of hydrogen and helium on these worlds is itself a consequence of the strong Jovian gravity. The Jovian planets are massive enough to have retained even the lightest gas, hydrogen, and very little of their original atmospheres have escaped since the birth of the solar system 4.6 billion years ago. At the heart of each Jovian planet lies a dense, compact core many times more massive than Earth. • None of the Jovian planets has a solid surface of any kind. Their gaseous atmospheres just become denser with depth because of the pressure of the overlying layers, eventually becoming liquid in the interior. The surface we see from Earth is simply the top of the outermost layer of atmospheric clouds.
  • 6. JUPITER’S ATMOSPHERE • The atmosphere of Jupiter is the largest planetary atmosphere in the Solar System. It is mostly made of molecular hydrogen and helium in roughly solar proportions; other chemical compounds are present only in small amounts and include methane, ammonia, hydrogen sulfide and water. Although water is thought to reside deep in the atmosphere, its directly measured concentration is very low. The oxygen, nitrogen, sulfur, and noble gas abundances in Jupiter's atmosphere exceed solar values by a factor of about three. • The Jovian atmosphere shows a wide range of active phenomena, including band instabilities, vortices (cyclones and anticyclones), storms and lightning.The vortices reveal themselves as large red, white or brown spots (ovals). The largest two spots are the Great Red Spot(GRS) and Oval BA which is also red. These two and most of the other large spots are anticyclonic. Smaller anticyclones tend to be white. Vortices are thought to be relatively shallow structures with depths not exceeding several hundred kilometers. Located in the southern hemisphere, the GRS is the largest known vortex in the Solar System. It could engulf several Earths and has existed for at least three hundred years. Oval BA, south of GRS, is a red spot a third the size of GRS that formed in 2000 from the merging of three white ovals.
  • 7. THE ATMOSPHERE OF THE OUTER JOVIAN WORLDS • The atmospheres of Jupiter and Saturn are made almost entirely of hydrogen and helium, although there is some evidence they contain hydrogen compounds. Uranus and Neptune are made primarily of hydrogen compounds, with smaller traces of hydrogen, helium, metal and rock. The most common hydrogen compounds are methane (CH4), ammonia (NH3), and water (H2O). • The farther away a planet is from the Sun, the cooler its atmosphere will be. This means that the same gases will condense to form clouds at different altitudes on different planets because the condensation of a gas requires a specific amount of pressure and temperature. Ammonia, ammonium hydrosulfide and water make up the 3 cloud layers of Jupiter and Saturn. You can see from the graph to the right that these condense at lower altitudes in Saturn's atmosphere than they do in Jupiter's atmosphere.