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courses:phy100:5 [2023/08/16 10:39] – [4.2 Giant planets] asadcourses:phy100:5 [2023/11/05 22:43] (current) – [4.2 Giant planets] asad
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 We talk about this planet in detail because we know most about it and also because it is our home. The inner and outer composition of the earth will tell us a lot of things about planets in general. We talk about this planet in detail because we know most about it and also because it is our home. The inner and outer composition of the earth will tell us a lot of things about planets in general.
  
-{{https://www.nasa.gov/sites/default/files/images/297755main_GPN-2001-000009_full.jpg?nolink&600}}+{{https://upload.wikimedia.org/wikipedia/commons/thumb/a/a8/NASA-Apollo8-Dec24-Earthrise.jpg/768px-NASA-Apollo8-Dec24-Earthrise.jpg?nolink&500}}
  
 The earth also became an astronomical object in the 1960s when the Apollo missions took pictures of the earth from the moon and the earth became another object in the sky for us. The first picture of the earth rising above the moon is shown above. It was taken by Apollo 8 astronauts in 1968. The earth also became an astronomical object in the 1960s when the Apollo missions took pictures of the earth from the moon and the earth became another object in the sky for us. The first picture of the earth rising above the moon is shown above. It was taken by Apollo 8 astronauts in 1968.
  
-{{https://www.nasa.gov/sites/default/files/images/608134main_world-orig_full.jpg?nolink&500}}+{{https://upload.wikimedia.org/wikipedia/commons/thumb/6/61/608134main_world-orig_full.jpg/767px-608134main_world-orig_full.jpg?nolink&500}}
  
 The interior of the earth is as complex as that of the sun. It has a 'solid' inner core, a liquid outer core, a mantle and a crust. The upper part of the mantle is almost like a liquid and the solid crust shakes and moves on top of this liquid-like upper mantle. The inner core is made of solid iron, the outer core of liquid iron. Because of the motion of iron at the cores, a giant magnetic field is created that extends beyond the atmosphere of the earth and creates a **magnetosphere** as shown below. The interior of the earth is as complex as that of the sun. It has a 'solid' inner core, a liquid outer core, a mantle and a crust. The upper part of the mantle is almost like a liquid and the solid crust shakes and moves on top of this liquid-like upper mantle. The inner core is made of solid iron, the outer core of liquid iron. Because of the motion of iron at the cores, a giant magnetic field is created that extends beyond the atmosphere of the earth and creates a **magnetosphere** as shown below.
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 {{:courses:phy100:terrestrial-planets-atmospheres.png?nolink|}} {{:courses:phy100:terrestrial-planets-atmospheres.png?nolink|}}
  
-The Moon and the Mercury do not have atmospheres, but the Earth, Mars and Venus do. The atmospheres of Mars and Venus are dominated by $CO_2$ (carbon-di-oxide), but the atmosphere of Earth is rich in nitrogen ($N_2$) and oxygen ($O_2$).+The Moon and the Mercury do not have atmospheres, but the Earth, Mars and Venus do. The atmospheres of Mars and Venus are dominated by $CO_2$ (carbon-di-oxide), but the atmosphere of Earth is rich in nitrogen ($N_2$) and oxygen ($O_2$). The clouds of Earth are made of frozen water, the clouds of Mars are made of CO$_2$, but the clouds of Venus are made of poisonous sulfuric acid. The surface of Venus is flooded with acid rain.
  
 Mercury is the closest to the sun, but Venus has the highest atsmospheric temperature (500 $^\circ$C) because of excessive greenhouse effect in its atmosphere. Average temperature on the surface of the earth is 287 kelvin or 14 degrees Celsius, and it keeps decreasing as you go toward Mars. Mercury is the closest to the sun, but Venus has the highest atsmospheric temperature (500 $^\circ$C) because of excessive greenhouse effect in its atmosphere. Average temperature on the surface of the earth is 287 kelvin or 14 degrees Celsius, and it keeps decreasing as you go toward Mars.
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 One very interesting fact is that the earth is smaller than the cores of these planets. Each of the giant planets harbor a solid sphere the size of the earth at their center. One very interesting fact is that the earth is smaller than the cores of these planets. Each of the giant planets harbor a solid sphere the size of the earth at their center.
  
 +{{gallery>:img:planets}}
 ==== - The moons ==== ==== - The moons ====
-Only Earth and Mars among the terrestrial planets have moons, or natural satellites. Our moon is the 'moon', but the natural satellites of other planets are sometimes also called 'a moon'. Almost 300 moons have been discovered. Any object orbiting a planet is a moon no matter how small. But only a few of the moons are big enough to be completely round in shape.+Only Earth and Mars among the terrestrial planets have moons, or natural satellites. Our moon is the 'moon', but the natural satellites of other planets are sometimes also called 'a moon'. Almost 300 moons have been discovered. Any object orbiting a planet is a moon no matter how small. But only 19 of the almost 300 moons are big enough to be completely round in shape because of their self-gravity.
  
 {{:courses:phy100:moons.jpg?nolink|}} {{:courses:phy100:moons.jpg?nolink|}}
courses/phy100/5.1692203971.txt.gz · Last modified: 2023/08/16 10:39 by asad
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