Chapter 7d Hothouse Venus. Venus Orbital distance: –108 200 000 km (0.72 AU) –NOT Eccentric Year: –224.7 d Day: –-243.018 d –Retrograde rotation Temperature:

Slides:



Advertisements
Similar presentations
Chapter 27.3 The Inner Planets
Advertisements

Venus: Global warming gone bad. Earth & Venus: Sister planets? VenusEarth Mass5x10 24 kg6x10 24 kg a (semi- major axis) 0.7 AU1 AU T at surface~750 K~300.
Chapter 7 Earth and the Terrestrial Worlds
Chapter 7 Earth and the Terrestrial Worlds
Atmospheres of the Terrestrial Planets. Atmospheres of the Moon and Mercury The Moon Mercury There is no substantial atmosphere on either body.
Chapter 7 Earth and the Terrestrial Worlds. Mercury craters smooth plains, cliffs.
Clicker Questions Chapter 6 The Terrestrial Planets Copyright © 2010 Pearson Education, Inc.
The Inner Planets. The Inner Planets to Scale 3,031 mi 7,521 mi 7,926 mi 4,222 mi 5.4 g/cm3 5.2 g/cm3 5.5 g/cm3 3.9 g/cm^3.
Venus and Mercury. The Inner Planets Venus Only a bit smaller than Earth Nearest planet (26 million miles) Shows phases as it orbits the Sun Most circular.
Chapter 28 Venus Copyright (c) The McGraw-Hill Companies, Inc. Permission required for reproduction or display.
ASTR100 (Spring 2008) Introduction to Astronomy Earth as a Planet Prof. D.C. Richardson Sections
Venus. Venus Data Guiding Questions 1.What makes Venus such a brilliant “morning star” or “evening star”? 2.What is strange about the rotation of Venus?
METO 637 Lesson 21. Mars Much of the surface is very old and cratered but there are also younger rift valleys, ridges, hills and plains. No plate tectonics.
Plate tectonics Image from
Mercury, seen from Earth through a moderate telescope.
Planetary Atmospheres (Chapter 10). Based on Chapter 10 This material will be useful for understanding Chapters 11 and 13 on “Jovian planet systems” and.
Astronomy190 - Topics in Astronomy Astronomy and Astrobiology Lecture 11 : Earth’s Habitability Ty Robinson.
Astronomy Picture of the Day. Mercury Mass = M Earth Radius = 0.38 R Earth  Surface Temp: K Average distance from Sun =.39 AU Moonlike:
Astronomy Picture of the Day. Mercury Mass = M Earth Radius = 0.38 R Earth  Surface Temp: K Moonlike: Surface craters, no atmosphere.
Understanding Our Atmosphere
Venus The bright and morning (evening) star. Moon & Venus Morning of April 22, 2009
Chapter 9: Venus Often called Earth’s sister planet because of their comparable sizes, Venus is actually nothing like our own world. Surface conditions.
Lecture Outlines Astronomy Today 8th Edition Chaisson/McMillan © 2014 Pearson Education, Inc. Chapter 9.
Chapter 16 Section 3 Inner Planets.
The Solar System.
Chapter 6 The Terrestrial Planets. Units of Chapter 6 Orbital and Physical Properties Rotation Rates Atmospheres The Surface of Mercury The Surface of.
11b. Cloud-Covered Venus The Venusian atmosphere Venus has slow retrograde rotation Venus has a hot dense atmosphere Volcanic eruptions form Venusian clouds.
Lecture 19. Outline Discuss Quiz Mercury Venus Outline For Rest of Semester Oct. 29 th Chapter 9 (Earth) Nov 3 rd and 5 th Chapter 9 and Chapter 10 (Earth.
Chapter 7e Earth is a living planet. 7.5 Earth as a Living Planet Our Goals for Learning What unique features on Earth are important for human life? How.
The Goldilocks Problem?. Astronomical! Why is Venus so hot…
The planet Venus was named after the goddess of love and beauty; Aphrodite. Venus is the brightest of the planets known. Like the moon, Venus shows phases.
Handout 27-3 The Inner Planets.
Unit 2 Lesson 4 The Terrestrial Planets Copyright © Houghton Mifflin Harcourt Publishing Company.
Lecture 35. Habitable Zones. reading: Chapters 9, 10.
(Terrestrial) Planetary Atmospheres II.  Atmospheres consist of exospheres only  Take either of their atmospheres, could “almost store them in a dorm.
1 Inner or Terrestrial Planets All the inner planets formed at the same time. Their composition is also very similar. They lack the huge atmospheres of.
Global Warming and the Venus Greenhouse Effect 24 February 2015.
Chapter 27 Planets of the Solar System 27.3 The Inner Planets
The Inner Planets 1. Mercury 2. Venus 3. Earth 4. Mars The inner planets are relatively small and rocky. They are known as “terrestrial” planets.
Venus By: Shahrukh and Michael. Geological Features ► We find evidence for many of the same geological features found on Earth: canyons, volcanoes, lava.
Cloud-Covered Venus Chapter Twelve.
The Inner Planets Chapter Terrestrial Planets Mercury, Venus, Earth, Mars Mostly solid rock with metallic cores Impact craters.
Gaia (or other spellings) is generally accepted as a mythical Greek name for Earth. No one really know, for sure, where the name “Earth” came from.
1 Venus vs. Earth In bulk, Venus and Earth are twin worlds.  nearly the same size  nearly the same density This similarity leads to an expectation of.
Full name Period III. Chapter 14, section 3: The Inner Planets A. The inner planets: are the four terrestrial planets that are closest to the sun. Mercury.
VENUS. “Twin” or “Sister” planet of the earth  similar size, mass, density; interior should also be similar with iron core, mantle, crust But totally.
Earth and the Other Terrestrial Worlds
The Inner Planets.
Chapter 7b Geologically Dead! Images from
EXPLAIN THE NEBULAR HYPOTHESIS OF THE ORIGIN OF THE SOLAR SYSTEM. DESCRIBE HOW THE PLANETS FORMED DESCRIBE THE FORMATION OF THE LAND, THE ATMOSPHERE, AND.
Astronomy: A Beginner’s Guide to the Universe Seventh Edition © 2013 Pearson Education, Inc. Chapter 6 Lecture The Terrestrial Planets.
What are the Inner planets?
Venus Goddess Of Love and Beauty. Venus is… Venus is the second planet from the Sun (67.24 million miles). it has 0 moons. A full day on Venus would be.
Unit 11 Mars. Physical Properties Radius: 3400 km Moons: Deimos, Phobos Mass: 6.4 × kg Density: 3900 kg/m 3 Length of Day: 24.6 hours.
By. Tommy Bell and Colton Reed The Solar System. Mercury 1. Is the closet planet to the sun 2. Its orbit takes 88 days and is the shortest of all the.
Chapter 7c Mars: Freeze-dried Image from:
PLANETS What is an AU? An astronomical unit (AU) is the average distance of the Earth from the sun. 1 AU = 150 million kilometers.
THE INNER PLANETS. WHAT DO THEY ALL HAVE IN COMMON? Q : Which planet is largest? Q : Which planet has the most moons? Q : Which planet is most similar.
The Terrestrial Planets Chapter 23, Section 2. Mercury: The Innermost Planet  Mercury, the innermost and smallest planet (not counting Pluto), is hardly.
Copyright © 2010 Pearson Education, Inc. The Terrestrial Planets.
VENUS Venus was named for the Goddess of love and beauty llan.jpg.
© 2010 Pearson Education, Inc. Erosion of Craters Details of some craters suggest they were once filled with water.
27-3OBJECTIVES Identify the basic characteristics of the inner planets. Compare the characteristics of the inner planets. Summarize the features that allow.
Venus Mass = 0.82 MEarth Radius = 0.95 REarth Density = 5.2 g/cm3
Atmospheric History of Venus
Comparing the atmospheres of Venus, Earth, and Mars
11b. Cloud-Covered Venus The Venusian atmosphere
Rising Carbon Dioxide Levels
Comparing the atmospheres of Venus, Earth, and Mars
Venus.
Presentation transcript:

Chapter 7d Hothouse Venus

Venus Orbital distance: – km (0.72 AU) –NOT Eccentric Year: –224.7 d Day: – d –Retrograde rotation Temperature: –Max: 475 o C 887 degrees Fahrenheit –Min: 450 o C 842 degrees Fahrenheit Diameter: – km Density: –5.204 g/cm 3 Composition: –Uncertain, but seems similar to Earth –Very dense atmosphere Axial Tilt: o Moons: none Other: –No magnetic field, possibly due to slow rotation

7.4 Venus: A Hothouse World Our Goals for Learning Is Venus geologically active? Why is Venus so hot?

Is Venus geologically active?

Radar images show lots of volcanic & tectonic features, as expected for a large terrestrial planet

Why is Venus so hot? Greenhouse effect. But why is it so prominent on Venus?

Thick CO 2 atmosphere of Venus locks heat in

Where is Earth’s CO 2 ?

Rocks - like limestone (and some in plant life and in the ocean) Why did this happen on Earth and not on Venus? Venus lacks oceans to dissolve the carbon dioxide and lock it away in rock on the seafloor And why is that?

We can understand Venus’ history by thinking about what would happen if Earth were moved to Venus’ orbit. How would the initial heating affect the oceans and the greenhouse effect?

A runaway greenhouse effect would then occur. Eventually, water molecules would break down & escape to space, just as apparently happened on Venus

What have we learned? Is Venus geologically active? Venus almost certainly remains geologically active today. Its surface shows evidence of major volcanic or tectonic activity in the past billion years, and it should retain nearly as much internal heat as Earth. However, geological activity on Venus differs from that on Earth in at least two key ways: lack of erosion and lack of plate tectonics. Why is Venus so hot? Venus’s extreme surface heat is a result of its thick, carbon dioxide atmosphere, which creates a very strong greenhouse effect. The reason Venus has such a thick atmosphere is its distance from the Sun: It was too close to develop liquid oceans like those on Earth, where most of the outgassed carbon dioxide dissolved in water and became locked away in rock. Thus, the carbon dioxide remained in the atmosphere, creating the strong greenhouse effect.