Top Banner
© 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacec
53

© 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

Dec 24, 2015

Download

Documents

Welcome message from author
This document is posted to help you gain knowledge. Please leave a comment to let me know what you think about it! Share it to your friends and learn new things together.
Transcript
Page 1: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

Planets and ExoPlanets

Earth, as viewed by the Voyager spacecraft

Page 2: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

What does the solar system look like?

Page 3: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

• There are eight major planets with nearly circular orbits.

• Pluto and Eris are smaller than the major planets and have more elliptical orbits.

Page 4: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

What are the major features of the Sun and planets?

Sun and planets to scale

Page 5: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

• Over 99.9% of solar system’s mass• Made mostly of H/He gas (plasma)• Converts 4 million tons of mass into energy each second

Sun

Page 6: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

• Made of metal and rock; large iron core • Desolate, cratered; long, tall, steep cliffs• Very hot and very cold: 425C (day)–170C (night)

Mercury

Page 7: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

• Nearly identical in size to Earth; surface hidden by clouds • Hellish conditions due to an extreme greenhouse effect• Even hotter than Mercury: 470C, day and night

Venus

Page 8: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

• An oasis of life• The only surface liquid water in the solar system• A surprisingly large moon

Earth and Moon with sizes shown to scale

Earth

Page 9: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

• Looks almost Earth-like, but don’t go without a spacesuit!• Giant volcanoes, a huge canyon, polar caps, more• Water flowed in distant past; could there have been life?

Mars

Page 10: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

• Much farther from Sun than inner planets

• Mostly H/He; no solid surface

• 300 times more massive than Earth

• Many moons, rings

Jupiter

Page 11: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

Jupiter’s moons can be as interesting as planets themselves, especially Jupiter’s four Galilean moons.

• Io (shown here): active volcanoes all over• Europa: possible subsurface ocean• Ganymede: largest moon in solar system• Callisto: a large, cratered “ice ball”

Page 12: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

Saturn

• Giant and gaseous like Jupiter• Spectacular rings• Many moons, including cloudy Titan

Page 13: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

Rings are NOT solid; they are made of countless small chunks of ice and rock, each orbiting like a tiny moon.

Artist’s conception

Page 14: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

Cassini probe arrived July 2004 (launched in 1997).

Page 15: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

• Smaller than Jupiter/Saturn; much larger than Earth

• Made of H/He gas and hydrogen compounds (H2O, NH3, CH4)

• Extreme axis tilt• Moons and rings

Uranus

Page 16: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

• Similar to Uranus (except for axis tilt)

• Many moons (including Triton)

Neptune

Page 17: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

Pluto (and Other Dwarf Planets)

• Much smaller than major planets• Icy, comet-like composition• Pluto’s main moon (Charon) is of similar size

Page 18: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

Motion of Large Bodies

• All large bodies in the solar system orbit in the same direction and in nearly the same plane.

• Most also rotate in that direction.

Page 19: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

Two Major Planet Types

• Terrestrial planets are rocky, relatively small, and close to the Sun.

• Jovian planets are gaseous, larger, and farther from the Sun.

Page 20: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

Swarms of Smaller Bodies

• Many rocky asteroids and icy comets populate the solar system.

Page 21: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

Notable Exceptions

• Several exceptions to the normal patterns need to be explained.

Page 22: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

Why is it so difficult to detect planets around other stars?

Page 23: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

Brightness Difference

• A Sun-like star is about a billion times brighter than the light reflected from its planets.

• This is like being in San Francisco and trying to see a pinhead 15 meters from a grapefruit in Washington, D.C.

Page 24: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

Planet Detection

• Direct: pictures or spectra of the planets themselves

• Indirect: measurements of stellar properties revealing the effects of orbiting planets

Page 25: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

How do we detect planets around other stars?

Page 26: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

Gravitational Tugs

• The Sun and Jupiter orbit around their common center of mass.

• The Sun therefore wobbles around that center of mass with same period as Jupiter.

Page 27: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

Gravitational Tugs

• The Sun’s motion around the solar system’s center of mass depends on tugs from all the planets.

• Astronomers around other stars that measured this motion could determine the masses and orbits of all the planets.

Page 28: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

Astrometric Technique

• We can detect planets by measuring the change in a star’s position on sky.

• However, these tiny motions are very difficult to measure (~ 0.001 arcsecond).

Page 29: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

Doppler Technique

• Measuring a star’s Doppler shift can tell us its motion toward and away from us.

• Current techniques can measure motions as small as 1 m/s (walking speed!).

Page 30: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

First Extrasolar Planet

• Doppler shifts of the star 51 Pegasi indirectly revealed a planet with 4-day orbital period.

• This short period means that the planet has a small orbital distance.

• This was the first* extrasolar planet to be discovered (1995).

Insert TCP 6e Figure 13.4a unannotatedInsert TCP 6e Figure 13.4a unannotated

Page 31: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

First Extrasolar Planet

• The planet around 51 Pegasi has a mass similar to Jupiter’s, despite its small orbital distance.

Insert TCP 6e Figure 13.4bInsert TCP 6e Figure 13.4b

Page 32: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

Other Extrasolar Planets

• Doppler shift data tell us about a planet’s mass and the shape of its orbit.

Page 33: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

Planet Mass and Orbit Tilt

• We cannot measure an exact mass for a planet without knowing the tilt of its orbit, because Doppler shift tells us only the velocity toward or away from us.

• Doppler data give us lower limits on masses.

Page 34: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

Transits and Eclipses

• A transit is when a planet crosses in front of a star.• The resulting eclipse reduces the star’s apparent

brightness and tells us planet’s radius.• No orbital tilt: accurate measurement of planet mass

Page 35: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

Spectrum During Transit

• Change in spectrum during a transit tells us about the composition of planet’s atmosphere.

Page 36: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

Surface Temperature Map

• Measuring the change in infrared brightness during an eclipse enables us to map a planet’s surface temperature.

Page 37: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

Direct Detection

• Special techniques like adaptive optics are helping to enable direct planet detection.

Page 38: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

Direct Detection

• Techniques that help block the bright light from stars are also helping us to find planets around them.

Page 39: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

Direct Detection

• Techniques that help block the bright light from stars are also helping us to find planets around them.

Page 40: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

Other Planet-Hunting Strategies

• Gravitational Lensing: Mass bends light in a special way when a star with planets passes in front of another star.

• Features in Dust Disks: Gaps, waves, or ripples in disks of dusty gas around stars can indicate presence of planets.

Page 41: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

What have we learned about extrasolar planets?

Page 42: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

Orbits of Extrasolar Planets

• Most of the detected planets have orbits smaller than Jupiter’s.

• Planets at greater distances are harder to detect with the Doppler technique.

Page 43: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

Orbits of Extrasolar Planets

• Orbits of some extrasolar planets are much more elongated (have a greater eccentricity) than those in our solar system.

Page 44: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

Multiple-Planet Systems

• Some stars have more than one detected planet.

Page 45: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

Orbits of Extrasolar Planets

• Most of the detected planets have greater mass than Jupiter.

• Planets with smaller masses are harder to detect with Doppler technique.

Page 46: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

Hot Jupiters

Page 47: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

Revisiting the Nebular Theory

• The nebular theory predicts that massive Jupiter-like planets should not form inside the frost line (at << 5 AU).

• The discovery of hot Jupiters has forced reexamination of nebular theory.

• Planetary migration or gravitational encounters may explain hot Jupiters.

Page 48: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

Planetary Migration

• A young planet’s motion can create waves in a planet-forming disk.

• Models show that matter in these waves can tug on a planet, causing its orbit to migrate inward.

Page 49: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

Orbital Resonances

• Resonances between planets can also cause their orbits to become more elliptical.

Page 50: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

Planets: Common or Rare?

• One in ten stars examined so far have turned out to have planets.

• The others may still have smaller (Earth-sized) planets that current techniques cannot detect.

• Kepler seems to indicate COMMON

Page 51: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

Transit Missions

• NASA’s Kepler mission was launched in 2008 to begin looking for transiting planets.

• It is designed to measure the 0.008% decline in brightness when an Earth-mass planet eclipses a Sun-like star.

Page 52: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

Astrometric Missions

• GAIA: a European mission planned for 2011 that will use interferometry to measure precise motions of a billion stars

• SIM: A NASA mission that will use interferometry to measure star motions even more precisely (to 10-6 arcseconds)

Page 53: © 2010 Pearson Education, Inc. Planets and ExoPlanets Earth, as viewed by the Voyager spacecraft.

© 2010 Pearson Education, Inc.

Direct Detection• Determining whether

Earth-mass planets are really Earth-like requires direct detection.

• Missions capable of blocking enough starlight to measure the spectrum of an Earth-like planet are being planned.

Mission concept for NASA’sMission concept for NASA’sTerrestrial Planet Finder (TPF)Terrestrial Planet Finder (TPF)