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The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global Properties III. The Rossiter-McClaughlin Effect (Spectroscopic Transits)

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Page 1: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

The Transit Method: Results from the Ground

I. Results from individual transit search programsII. The Mass-Radius relationships (internal structure)

Global Properties

III. The Rossiter-McClaughlin Effect (Spectroscopic Transits)

Page 2: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

The first time I gave this lecture (2003) there were 2 transiting extrasolar planets.

There are now 127 transiting extrasolar planets detected from ground-based programs

First ones were detected by doing follow-up photometry of radial velocity planets. Now transit searches are discovering exoplanets

Page 3: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

Radial Velocity Curve for HD 209458

Period = 3.5 days

Msini = 0.63 MJupThe probability is 1 in 10 that a short period Jupiter will transit. HD 209458 was the 10th short period exoplanet searched for transits

Page 4: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

Charbonneau et al. (2000): The observations that started it all:

• Mass = 0.63 MJupiter

• Radius = 1.35 RJupiter

• Density = 0.38 g cm–3

Page 5: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

Hubble Space Telescope.

An amateur‘s light curve.

Page 6: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

The OGLE Planets

• OGLE: Optical Gravitational Lens Experiment (http://www.astrouw.edu.pl/~ogle/)

• 1.3m telescope looking into the galactic bulge

• Mosaic of 8 CCDs: 35‘ x 35‘ field

• Typical magnitude: V = 15-19

• Designed for Gravitational Microlensing

• First planet discovered with the transit method

Page 7: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

The first planet found with the transit method

Page 8: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

Konacki et al.

Page 9: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

K = 510 ± 170 m/s

i= 79.8 ± 0.3

a= 0.0308

Mass = 4.5 MJ

Radius = 1.6 RJ

Spectral Type Star = F3 V

Vsini = 40 km/s

OGLE transiting planets: These produce low quality transits, they are faint, and they take up a large

amount of 8m telescope time..

Page 10: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

Planet Mass

(MJup)

Radius

(RJup)

Period

(Days)

Year

OGLE2-TR-L9 b 4.5 1.6 2.48 2007

OGLE-TR-10 b 0.63 1.26 3.19 2004

OGLE-TR-56 b 1.29 1.3 1.21 2002

OGLE-TR-111 b 0.53 1.07 4.01 2004

OGLE-TR-113 b 1.32 1.09 1.43 2004

OGLE-TR-132 b 1.14 1.18 1.69 2004

OGLE-TR-182 b 1.01 1.13 3.98 2007

 OGLE-TR-211 b 1.03 1.36 3.68 2007

Prior to OGLE all the RV planet detections had periods greater than about 3 days.

The last OGLE planet was discovered in 2007. Most likely these will be the last because the target stars are too faint.

The OGLE Planets

Page 11: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

The TrES Planets

• TrES: Trans-atlantic Exoplanet Survey (STARE is a member of the network http://www.hao.ucar.edu/public/research/stare/)

• Three 10cm telescopes located at Lowell Observtory, Mount Palomar and the Canary Islands

• 6.9 square degrees

• 5 Planets discovered

Page 12: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

TrEs 2b

P = 2.47 d

M = 1.28 MJupiter

R = 1.24 RJupiter

i = 83.9 deg

Page 13: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

Report that the transit duration is increasing with time, i.e. the inclination is changing:

However, Kepler shows no change in the inclination!

Discrepancy most likely due to wavelength depedent limb darkening

Page 14: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

The HAT Planets

• HATNet: Hungarian-made Automated Telescope (http://www.cfa.harvard.edu/~gbakos/HAT/

• Six 11cm telescopes located at two sites: Arizona and Hawaii

• 8 x 8 square degrees

• 36 Planets discovered

Page 15: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

HAT-P-12b

Star = K4 VPlanet Period = 3.2 days

Planet Radius = 0.96 RJup

Planet Mass = 0.21 MJup (~MSat)= 0.3 gm cm–3

The best fitting model for HAT-P-12b has a core mass ≤ 10 Mearth and is still dominated by H/He (i.e. like Saturn and Jupiter and not like Uranus and Neptune). It is the lowest mass H/He dominated gas giant planet.

Page 16: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

The WASP Planets

WASP: Wide Angle Search for Planets (http://www.superwasp.org). Also known as SuperWASP

• Array of 8 Wide Field Cameras

• Field of View: 7.8o x 7.8o

• 13.7 arcseconds/pixel

• Typical magnitude: V = 9-13

• 2 sites: La Palma, South Africa

• 65 transiting planets discovered so far

In a field of 400.000 stars WASP finds 12 candidates for a rate of 1 in 30.000 stars. If 10% are real planets the rate is 1 planet for every 300.000

Page 17: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

The First WASP Planet

Page 18: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

CoordinatesRA 00:20:40.07 Dec +31:59:23.7

Constellation Pegasus

Apparent Visual Magnitude 11.79

Distance from Earth 1234 Light Years

WASP-1 Spectral Type F7V

WASP-1 Photospheric Temperature

6200 K

WASP-1b Radius 1.39 Jupiter Radii

WASP-1b Mass 0.85 Jupiter Masses

Orbital Distance 0.0378 AU

Orbital Period 2.52 Days

Atmospheric Temperature 1800 K

Mid-point of Transit 2453151.4860 HJD

Page 19: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

WASP 12b: The Hottest Transiting Giant Planet

Discovery data

High quality light curve for accurate parameters

Doppler confirmation

Orbital Period: 1.09 d

Transit duration: 2.6 hrs

Planet Mass: 1.41 MJupiter

Planet Radius: 1.79 RJupiter

Planet Temperature: 2516 K

Spectral Type of Host Star: F7 V

Page 20: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

Mass: 60 MJupiter

Radius: ~1 RJupiter

Teff: ~ 2800 K

Planet Mass: 1.41 MJupiter

Planet Radius: 1.79 RJupiter

Planet Temperature: 2516 K

Comparison of WASP 12 to an M8 Main Sequence Star

WASP 12 has a smaller mass, larger radius, and comparable effective temperature than an M8 dwarf. Its atmosphere should look like an M9 dwarf or L0 brown dwarf. One difference: above temperature for the planet is only on the day side because the planet does not generate its own energy

Page 21: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

Although WASP-33b is closer to the planet than WASP-12 it is not as hot because the host star is cooler (4400 K) and it has a smaller radius

Page 22: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

GJ 436: The First Transiting Neptune

Host Star:

Mass = 0.4 Mּס (M2.5 V)

Butler et al. 2004

Page 23: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

„Photometric transits of the planet across the star are ruled out for gas giant compositions and are also unlikely for solid compositions“

Special Transits: GJ 436

Butler et al. 2004

Page 24: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

The First Transiting Hot Neptune!

Gillon et al. 2007

Page 25: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

Star  

Stellar mass [  Mּס  ] 0.44 (  ± 0.04)  

Planet  

Period [days] 2.64385 ±   0.00009  

Eccentricity 0.16 ±   0.02  

Orbital inclination 86.5   0.2

Planet mass [ ME  ] 22.6 ±   1.9

Planet radius [ RE  ] 3.95 +0.41-0.28

GJ 436

Mean density = 1.95 gm cm–3, slightly higher than Neptune (1.64)

Page 26: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

M = 3.11 MJup

HD 17156: An eccentric orbit planet

Probability of a transit ~ 3%

Page 27: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

R = 0.96 RJup

Barbieri et al. 2007

Mean density = 4.88 gm/cm3

Mean for M2 star ≈ 4.3 gm/cm3

Page 28: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

HD 80606: Long period and eccentric

a = 0.45 AU

dmin = 0.03 AU dmax = 0.87 AU

R = 1.03 RJup = 4.44 (cgs)

Probability of having a favorable orbital orientation is only 1%!

Page 29: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

D Charbonneau et al. Nature 462, 891-894 (2009) doi:10.1038/nature08679

MEarth-1b: A transiting Superearth

Page 30: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

D Charbonneau et al. Nature 462, 891-894 (2009) doi:10.1038/nature08679

Change in radial velocity of GJ1214.

Page 31: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

= 1.87 (cgs)

Neptune like

Page 32: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

So what do all of these transiting planets tell us?

= 1.24 gm/cm3 = 0.62 gm/cm3

= 1.25 gm/cm3 1.6 gm/cm3

5.5 gm/cm3

Page 33: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

Solar System Object (gm cm–3)

Mercury 5.43

Venus 5.24

Earth 5.52

Mars 3.94

Jupiter 1.24

Saturn 0.62

Uranus 1.25

Neptune 1.64

Pluto 2

Moon 3.34

Carbonaceous Meteorites

2–3.5

Iron Meteorites 7–8

Comets 0.06-0.6

The density is the first indication of the internal structure of the exoplanet

Rocks

He/H

Ice

Page 34: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

D Charbonneau et al. Nature 462, 891-894 (2009) doi:10.1038/nature08679

Masses and radii of transiting planets.

GJ 1214b is shown as a red filled circle (the 1σ uncertainties correspond to the size of the symbol), and the other known transiting planets are shown as open red circles. The eight planets of the Solar System are shown as black diamonds. GJ  1214b and CoRoT-7b are the only extrasolar planets with both well-determined masses and radii for which the values are less than those for the ice giants of the Solar System. Despite their indistinguishable masses, these two planets probably have very different compositions. Predicted16 radii as a function of mass are shown for assumed compositions of H/He (solid line), pure H2O (dashed line), a hypothetical16 water-dominated world (75% H2O, 22% Si and 3% Fe core; dotted line) and Earth-like (67.5% Si mantle and a 32.5% Fe core; dot-dashed line). The radius of GJ 1214b lies 0.49 ± 0.13 R above the water-world curve, indicating that even if the planet is predominantly water in composition, it ⊕probably has a substantial gaseous envelope

H/He dominated

Pure H20

75% H20, 22% Si67.5% Si mantle

32.5% Fe

(earth-like)

Page 35: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

Take your favorite composition and calculate the mass-radius relationship

Page 36: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

Period = 2.87 d

Rp = 0.7 RJup

Mp = 0.36 MJup

Sato et al. 2005

HD 149026: A planet with a large core

Mean density = 2.8 gm/cm3

Page 37: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

~70 Mearth core mass is difficult to form with gravitational instability.

HD 149026 b provides strong support for the core accretion theory

Rp = 0.7 RJup

Mp = 0.36 MJup

Mean density = 2.8 gm/cm3

10-13 Mearth core

Page 38: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

Lower bound

= 0.15 gm cm–3

Upper bound

= 3 gm cm–3

Page 39: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

Planet Radius

Most transiting planets tend to be inflated. Approximately 68% of all transiting planets have radii larger than 1.1 RJup.

Page 40: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

Possible Explanations for the Large Radii

1. Irradiation from the star heats the planet and slows its contraction it thus will appear „younger“ than it is and have a larger radius

Models I, C, and D are for isolated planets

Models A and B are for irradiated planets.

Page 41: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

There is a slight correlation of radius with planet temperature (r = 0.37)

Page 42: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

Possible Explanations for the Large Radii

2. Slight orbital eccentricity (difficult to measure) causes tidal heating of core → larger radius

Slight Problem:

3. We do not know what is going on.

HD 17156b: e=0.68 R = 1.02 RJup

HD 80606b: e=0.93 R = 0.92 RJup

CoRoT 10b: e=0.53 R = 0.97RJup

Caveat: These planets all have masses 3-4 MJup, so it may be the smaller radius is just due to the larger mass.

Page 43: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

0

2

4

6

8

10

12

14

0.2 0.6 1.0 1.4 1.8 2.2 2.6 3.0

N

J/US N

Density Distribution

Density (cgs)

Nu

mb

er

Page 44: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

Comparison of Mean Densities of eccentric planets

Giant Planets with M < 2 MJup : 0.78 cgs

HD 17156, P = 21 d, e= 0.68 M = 3.2 MJup, density = 4.8

HD 80606, P = 111 d, e=0.93, M = 3.9 MJup, density = 4.4

CoRoT 10b, P=13.2, e= 0.53, M = 2.7 MJup, density = 3.7

The three eccentric transiting planets have high mass and high densities. Formed by mergers?

Page 45: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

0

2

4

6

8

10

12

14

16

0.25 1.75 3.25 4.75 6.25 7.75 9.25

Transits

RV

Period (Days)

Nu

mb

erPeriod Distribution for short period Exoplanets

p = 7%

p = 13%

p = probability of a favorable orbit

Page 46: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

The ≈ 3 day period may mark the inner edge of the proto-planetary disk

Both RV and Transit Searches show a peak in the Period at 3 days

Page 47: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

Mass-Radius Relationship

Radius is roughly independent of mass, until you get to small planets (rocks)

Rad

ius

(RJ)

Mass (MJ)

Page 48: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

Modified From H. Rauer

CoRoT-3b : Radius = Jupiter, Mass = 21.6 Jupiter

CoRoT-1b : Radius = 1.5 Jupiter, Mass = 1 Jupiter

OGLE-TR-133b: Radius = 1.33 Jupiter, Mass = 85 Jupiter

CoRoT-1b

CoRoT-3b

OGLE-TR-133b

Page 49: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

Planet Mass Distribution

Transiting Planets

RV Planets

Close in planets tend to have lower mass, as we have seen before.

Page 50: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

0

2

4

6

8

10

12

14

16

18

-0.45 -0.25 -0.05 0.15 0.35

Transits

[Fe/H]

Num

ber 0

10

20

30

40

50

60

70

-0.45 -0.25 -0.05 0.15 0.35

RV

Metallicity Distribution

[Fe/H] Doppler result: Recall that stars with higher metal content seem to have a higher frequency of planets. This is not seen in transiting planets.

Page 51: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

0

5

10

15

20

25

30

0.5 0.7 0.9 1.1 1.3 1.5

0

10

20

30

40

50

60

70

80

0.5 0.7 0.9 1.1 1.3 1.5

Host Star Mass Distribution

Stellar Mass (solar units)

Nu

mb

erTransiting Planets

RV Planets

Page 52: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

V- magnitude

Per

cen

t

Stellar Magnitude distribution of Exoplanet Discoveries

0,00%

5,00%

10,00%

15,00%

20,00%

25,00%

30,00%

35,00%

0.5 4,50 8,50 12,50 16,50

Transits

RV

Page 53: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

Summary of Global Properties of Transiting Planets

1. Transiting giant planets (close-in) tend to have inflated radii (much larger than Jupiter)

2. A significant fraction of transiting giant planets are found around early-type stars with masses ≈ 1.3 Msun.

3. There appears to be no metallicity-planet connection among transiting planets or at most a weak one.

4. The period distribution of close-in planets peaks around P ≈ 3 days for both RV and transit discovered planets.

5. Most transiting giant planets have densities near that of Saturn. It is not known if this is due to their close proximity to the star (i.e. inflated radius)

6. Transiting planets have been discovered around stars fainter than those from radial velocity surveys

Page 54: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

• Early indications are that the host stars of transiting planets have slightly different properties than non-transiting planets.

• Most likely explanation: Transit searches are not as biased as radial velocity searches. One looks for transits around all stars in a field, these are not pre-selected. The only bias comes with which ones are followed up with Doppler measurements

• Caveat: Transit searches are biased against smaller stars. i.e. the larger the star the higher probability that it transits

Page 55: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

Spectroscopic Transits:

The Rossiter-McClaughlin Effect

Page 56: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

The Rossiter-McClaughlin Effect

1

1

0

+v

–v

2

3

4

2 3 4

The R-M effect occurs in eclipsing systems when the companion crosses in front of the star. This creates a distortion in the normal radial velocity of the star. This occurs at point 2 in the orbit.

Page 57: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

From Holger Lehmann

The Rossiter-McLaughlin Effect in an Eclipsing Binary

Page 58: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

Curves show Radial Velocity after removing the binary orbital motion

The effect was discovered in 1924 independently by Rossiter and McClaughlin

Page 59: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global
Page 60: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

Spectral Type

Vequator (km/s)

O5 190

B0 200

B5 210

A0 190

A5 160

F0 95

F5 25

G0 12

Average rotational velocities in main sequence stars

Page 61: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

The Rossiter-McClaughlin Effect

–v +v

0

As the companion cosses the star the observed radial velocity goes from + to – (as the planet moves towards you the star is moving away). The companion covers part of the star that is rotating towards you. You see more possitive velocities from the receeding portion of the star) you thus see a displacement to + RV.

–v

+v

When the companion covers the receeding portion of the star, you see more negatve velocities of the star rotating towards you. You thus see a displacement to negative RV.

Page 62: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

The Rossiter-McClaughlin Effect

What can the RM effect tell you?

Planet

1) The orbital inclination or impact parameter

a

a2

a2

Page 63: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

The Rossiter-McClaughlin Effect

2) The direction of the orbit

Planet

b

Page 64: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

The Rossiter-McClaughlin Effect

2) The alignment of the orbit

Planet

cd

Page 65: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

What can the RM effect tell you?

3. Are the spin axes aligned?

Orbital plane

Page 66: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

Summary of Rossiter-McClaughlin „Tracks“

Page 67: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

Amplitude of the R-M effect:

ARV = m s–

1

Note:

1. The Magnitude of the R-M effect depends on the radius of the planet and not its mass.

2. The R-M effect is proportional to the rotational velocity of the star. If the star has little rotation, it will not show a R-M effect.

rRJup

( )2

RRּס

( )–2Vs

5 km s–1 ( )ARV is amplitude after removal of orbital mostion

Vs is rotational velocity of star in km s–1

r is radius of planet in Jupiter radii

R is stellar radius in solar radii

Page 68: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

= –0.1 ± 2.4 deg

HD 209458

Page 69: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

= –1.4 ± 1.1 deg

HD 189733

Page 70: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

HD 147506

Best candidate for misalignment is HD 147506 because of the high eccentricity

Page 71: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

Two possible explanations for the high eccentricities seen in exoplanet orbits:

• Scattering by multiple giant planets

• Kozai mechanism

On the Origin of the High Eccentricities

Page 72: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

Planet-Planet Interactions

Initially you have two giant planets in circular orbits

These interact gravitationally. One is ejected and the remaining planet is in an eccentric orbit

Page 73: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

Kozai Mechanism

Two stars are in long period orbits around each other.

A planet is in a shorter period orbit around one star.

If the orbit of the planet is inclined, the outer planet can „pump up“ the eccentricity of the planet. Planets can go from circular to eccentric orbits.

Page 74: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

Winn et al. 2007: HD 147506b (alias HAT-P-2b)

If either mechanism is at work, then we should expect that planets in eccentric orbits not have the spin axis aligned with the stellar rotation. This can be checked with transiting planets in eccentric orbits

Spin axes are aligned within 14 degrees (error of measurement). No support for Kozai mechanism or scattering

Page 75: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

What about HD 17156?

Narita et al. (2007) reported a large (62 ± 25 degree) misalignment between planet orbit and star spin axes!

Page 76: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

Cochran et al. 2008: = 9.3 ± 9.3 degrees → No misalignment!

Page 77: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

XO-3-b

Page 78: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

Hebrard et al. 2008

= 70 degrees

Page 79: The Transit Method: Results from the Ground I. Results from individual transit search programs II. The Mass-Radius relationships (internal structure) Global

Winn et al. (2009) recent R-M measurements for X0-3

= 37 degrees

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Fabricky & Winn, 2009, ApJ, 696, 1230

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= 182 deg!

HAT-P7

= 182 deg!

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HD 80606

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= 32-87 deg

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HARPS data : F. Bouchy Model fit: F. Pont Lambda ~ 80 deg!

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Distribution of spin-orbit axes

Red: retrograde orbits

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0

2

4

6

8

10

12

14

16

18

-160 -80 0 80 160

Number

35% of Short Period Exoplanets show significant misalignments

~10-20% of Short Period Exoplanets are in retrograde orbits

Basically all angles are covered

(deg)

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2.

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The Rossiter-McLaughlin Effect or „Rotation Effect“

For rapidly rotating stars you can „see“ the planet in the spectral line

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For stars whose spectral line profiles are dominated by rotational broadening there is a one to one mapping between location on the star and location in the line profile:

V = –Vrot V = +Vrot

V = 0

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For slowly rotationg stars you do not see the distortion, but you measure a radial velocity displacement due to the distortion.

A „Doppler Image“ of a Planet

Prograde orbit

Retrograd orbit

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HD 15082 = WASP-33

No RV variations are seen. A companion of radius 1.5 RJup is either a planet, brown dwarf, or low mass star. The RV variations exclude BD

and stellar companion.

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The Line Profile Variations of HD 15082 = WASP-33

Pulsations

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Summary

1. There are 2 ways from spectroscopy to measure the angle between the spin axis and the orbital axis of the star:

a) Rossiter-McClaughlin effect (most successful)

b) Doppler tomography

2. No technique can give you the mass

3. Exoplanets show all possible obliquity angles, but most are aligned (even in eccentric orbits)

4. Implications for planet formation (problems for migration theory)