© 2010 pearson education, inc. planets and exoplanets earth, as viewed by the voyager spacecraft

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

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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

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© 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)