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The Gas Giants Astronomy 311 Professor Lee Carkner Lecture 16.

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Presentation on theme: "The Gas Giants Astronomy 311 Professor Lee Carkner Lecture 16."— Presentation transcript:

1 The Gas Giants Astronomy 311 Professor Lee Carkner Lecture 16

2 Gas Giant Basics  The 4 largest planets of the solar system are the gas giants   

3 Missions to the Outer Planets  1972 Pioneer 10 --   1973 Pioneer 11 --  1977 Voyager 1 --  1977 Voyager 2 --  1989 Galileo --  1997 Cassini -- 

4 Voyager 2  Launched August 20 1977    Used gravity of each planet to change orbit to get to the next   Is still taking data on the edge of the solar system

5 Voyager 2’s Grand Tour

6 Gas Giant Facts  Jupiter  Diameter: 11.21  Mass: 317.83  Orbital Radius: 5.20  Saturn  Diameter: 9.42  Mass: 95.16  Orbital Radius: 9.54  Uranus  Diameter: 4.01  Mass: 14.50  Orbital Radius: 19.19  Neptune  Diameter: 3.88  Mass: 17.20  Orbital Radius: 30.06  Numbers are relative to the Earth

7 Orbits  Orbital radii for the outer planets range from ~5-30 AU   

8 Sizes of the Gas Giants  Gas giants are all very large compared to the terrestrial planets  Jupiter and Saturn about 10 Earth diameters   Uranus and Neptune about 4 Earth diameters   The gas giants contain 99% of the mass of the solar system (not including the Sun)  

9 Densities  The gas giants have very low densities  Average density (kg/m 3 )  Jupiter:  Saturn:  Uranus:  Neptune:  For comparison Earth’s density is 5515 

10 Composition  The gas giants have a low density because they are made up mostly of hydrogen and helium the 2 lightest elements    Total composition   

11 Surface and Atmosphere  The gas giants do not have a real “surface”  

12 Atmospheric Features  Clouds     Bands    Storms  

13 Jupiter’s Great Red Spot

14 Neptune’s Great Dark Spot

15 Hurricane on Earth

16 Saturn’s Atmosphere

17 Traveling Through the Solar System

18 Structure  The gas giants are not perfectly round, they are oblate due to rotation  Degree of oblateness depends on mass distribution   Gas giants also have a magnetic field 

19 Internal Structure of Jupiter

20 Moons   Number of satellites (larger than 10 km)      Range in size from Ganymede (larger then Mercury) to small pieces of rock

21 Moon Properties  Satellites tend to be composed of rock and ice   Many have rocky cores and icy surfaces  The satellites are very diverse:   

22 Jupiter’s Satellites

23 Saturn’s Satellites

24 Rings  All of the gas giants have rings of small particles    Rings consist of material that has fallen inside the Roche limit 

25 Saturn’s A Ring

26 Differences Between the Gas Giants  Jupiter and Saturn are larger,warmer and have more distinct cloud features  

27 Summary  Size: ~4-11 times Earth diameter  Mass: ~15-318 Earth masses  Composition: mostly hydrogen and helium  Atmosphere: clouds of methane and ammonia  also have large, long-lived storm systems and oppositely moving bands

28 Summary: The Jovian Systems  The gas giants have extensive satellite systems  Many moons have icy exteriors with rocky cores  Some are very large (~size of Earth’s Moon)  All of the outer planets (not just Saturn have ring systems)  rings composed of small particles  Ring properties different for each planet


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