chapter 9: venus. 9.1 orbital properties 9.2 physical properties 9.3 long-distance observations of...

Download Chapter 9: Venus. 9.1 Orbital Properties 9.2 Physical Properties 9.3 Long-Distance Observations of Venus 9.4 The Surface of Venus 9.5 The Atmosphere of

If you can't read please download the document

Upload: pauline-fletcher

Post on 24-Dec-2015

219 views

Category:

Documents


5 download

TRANSCRIPT

  • Slide 1
  • Chapter 9: Venus
  • Slide 2
  • 9.1 Orbital Properties 9.2 Physical Properties 9.3 Long-Distance Observations of Venus 9.4 The Surface of Venus 9.5 The Atmosphere of Venus 9.6 Venuss Magnetic Field and Internal Structure Units of Chapter 9
  • Slide 3
  • Venus is much brighter than Mercury, and can be farther from the Sun Called morning or evening star, as it is still tied to Sun Brightest object in the sky, after Sun and Moon 9.1 Orbital Properties
  • Slide 4
  • Apparent brightness of Venus varies, due to changes in phase and distance from Earth
  • Slide 5
  • Radius: 6000 km Mass: 4.9 x 10 24 kg Density: 5200 kg/m 3 Rotation period: 243 days, retrograde 9.2 Physical Properties
  • Slide 6
  • Slow, retrograde rotation of Venus results in large difference between solar day (117 Earth days) and sidereal day (243 Earth days); note that the solar day is a large fraction of the year, and the sidereal day is even longer than the year.
  • Slide 7
  • Dense atmosphere and thick clouds make surface impossible to see Surface temperature is about 730 Khotter than Mercury! 9.3 Long-Distance Observations of Venus
  • Slide 8
  • Even probes flying near Venus, using ultraviolet or infrared, can see only a little deeper into the clouds
  • Slide 9
  • Surface is relatively smooth Two continent-like features: Ishtar Terra and Aphrodite Terra No plate tectonics Mountains, a few craters, many volcanoes and large lava flows 9.4 The Surface of Venus
  • Slide 10
  • Surface mosaics of Venus
  • Slide 11
  • Surface maps of Venus, with Earth comparison
  • Slide 12
  • Slide 13
  • Ishtar Terra is one of two continent-sized features on the surface of Venus
  • Slide 14
  • The other is Aphrodite Terra
  • Slide 15
  • Lava has flowed from cracks on the surface
  • Slide 16
  • Volcanoes on Venus; most are shield volcanoes
  • Slide 17
  • Other volcanic features include lava domes and coronas
  • Slide 18
  • Impact craters on Venus, the largest named after Margaret Mead
  • Slide 19
  • Photographs of the surface, from the Venera landers
  • Slide 20
  • Venuss atmosphere is very dense Solid cloud bank 5070 km above surface Atmosphere is mostly carbon dioxide; clouds are sulfuric acid 9.5 The Atmosphere of Venus
  • Slide 21
  • Slide 22
  • Upper atmosphere of Venus has high winds, but atmosphere near surface is almost calm
  • Slide 23
  • There are also permanent vortices at the poles; the origin of the double-lobed structure is a mystery
  • Slide 24
  • Venus is the victim of a runaway greenhouse effectjust kept getting hotter and hotter as infrared radiation was reabsorbed
  • Slide 25
  • No magnetic field, probably because rotation is so slow No evidence for plate tectonics Venus resembles a young Earth (1 billion years)no asthenosphere, thin crust 9.6 Venuss Magnetic Field and Internal Structure
  • Slide 26
  • The rotational period of Venus was measured by A.watching surface features move across the planet's disk. B.measuring the speed of clouds in the planet's atmosphere. C.measuring the Doppler shift of radar signals bounded off the planet's surf. D.orbiting spacecraft around the planet.
  • Slide 27
  • How is it possible that Venus's surface may be hotter than Mercury's? A.It is closer to the sun. B.Venus's larger area absorbs more heat. C.Venus rotates in a retrograde direction. D.Venus's lack of atmosphere allows sunlight to hit the surface without reflection. E.Venus has quite a lot of carbon dioxide in its atmosphere.
  • Slide 28
  • The atmosphere near the surface of Venus is: A.almost completely opaque. B.nearly transparent. C.about like a dense fog on Earth. D.unknown since we have not explored the surface of Venus.
  • Slide 29
  • The fact that Venus has little or no magnetic field is attributed to A.its slow rotation. B.its cloud cover. C.its proximity to the sun. D.its proximity to Earth. E.the greenhouse effect.
  • Slide 30
  • Venus was once considered to be Earth's sister planet because: A.it is the closest planet to Earth. B.it is similar in size. C.it has a similar mass. D.it has an atmosphere. E.all of the above.
  • Slide 31
  • How does the surface pressure on Venus compare to that on the Earth? A.It is much less. B.It is about the same. C.It is much greater. D.It is negligible.
  • Slide 32
  • The temperature of the surface of Venus is closest to _____ degrees Fahrenheit. A.100 B.500 C.1,000 D.10,000
  • Slide 33
  • Detailed photographs of surface features of Venus: A.do not exist. B.exist as the result of venera photographs of a very few limited areas. C.exist in abundance because of robot landers. D.exist in abundance because astronauts and cosmonauts landed on the surface.
  • Slide 34
  • Venus is never too far from Sun and is the brightest object in the sky (after the Sun and Moon) Atmosphere very dense, mostly carbon dioxide Surface hidden by cloud cover Surface temperature 730 K Rotation slow and retrograde Summary of Chapter 9
  • Slide 35
  • Many lava domes and shield volcanoes Venus is comparable to Earth in mass and radius Large amount of carbon dioxide in atmosphere, and closeness to Sun, led to runaway greenhouse effect and very hot surface Summary of Chapter 9 (cont.)