1 The Transit Method: Results from the Ground Results from individual transit search programs The Mass-Radius relationships (internal structure) Global Properties The Rossiter-McClaughlin Effect
2 There are now 124 transiting extrasolar planets First ones were detected by doing follow-up photometry of radial velocity planets. Now transit searches are discovering exoplanets Transiting Exoplanets
3 Radial Velocity Curve for HD Period = 3.5 days Msini = 0.63 M Jup The probability is 1 in 10 that a short period Jupiter will transit. HD was the 10th short period exoplanet searched for transits
4 Charbonneau et al. (2000): The observations that started it all: Mass = 0.63 MJupiter Radius = 1.35 RJupiter Density = 0.38 g cm 3
5 An amateur s light curve. Hubble Space Telescope.
6 HD b has a radius larger than expected. Burrows et al Evolution of the radius of HD b and τ Boob HD b Models I, C, and D are for isolated planets Models A and B are for irradiated planets. One hypothesis for the large radius is that the stellar radiation hinders the contraction of the planet (it is hotter than it should be) so that it takes longer to contract. Another is tidal heating of the core of the planet if you have nonzero eccentricity
7 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 = Designed for Gravitational Microlensing First planet discovered with the transit method
8 The first planet found with the transit method
9 Konacki et al.
10 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.. K = 510 ± 170 m/s i= 79.8 ± 0.3 a= Mass = 4.5 M J Radius = 1.6 R J Spectral Type = F3 V
11 The OGLE Planets Planet Mass Radius Period (M Jup ) (R Jup ) (Days) OGLE2-TR-L9 b Year 2007 OGLE-TR-10 b OGLE-TR-56 b OGLE-TR-111 b OGLE-TR-113 b OGLE-TR-132 b OGLE-TR-182 b OGLE-TR-211 b Prior to OGLE all the RV planet detections had periods greater than about 3 days. The last OGLE planet was discovered in Most likely these will be the last because the target stars are too faint.
12 The TrES Planets TrES: Trans-atlantic Exoplanet Survey (STARE is a member of the network Three 10cm telescopes located at Lowell Observtory, Mount Palomar and the Canary Islands 6.9 square degrees 4 Planets discovered
13 TrEs 2b P = 2.47 d M = 1.28 M Jupiter R = 1.24 R Jupiter i = 83.9 deg
14 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 13 Planets discovered
15 HAT-P-12b Star = K4 V Planet Period = 3.2 days Planet Radius = 0.96 R Jup Planet Mass = 0.21 M Jup (~M Sat ) ρ = 0.3 g cm 3 The best fitting model for HAT-P-12b has a core mass 10 M earth 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.
16 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: 7.8 o x 7.8 o 13.7 arcseconds/pixel Typical magnitude: V = transiting planets discovered so far
17 The First WASP Planet
18 Coordinates RA 00:20:40.07 Dec +31:59:23.7 Constellation Pegasus Apparent Visual Magnitude Distance from Earth 1234 Light Years WASP-1 Spectral Type F7V WASP-1 Photospheric Temperature 6200 K WASP-1b Radius WASP-1b Mass Orbital Distance Orbital Period Atmospheric Temperature Mid-point of Transit 1.39 Jupiter Radii 0.85 Jupiter Masses AU 2.52 Days 1800 K HJD
19 WASP 12: Hottest Transiting Giant Planet Discovery data High quality light curve for accurate parameters Orbital Period: 1.09 d Transit duration: 2.6 hrs Planet Mass: 1.41 M Jupiter Doppler confirmation Planet Radius: 1.79 R Jupiter Planet Temperature: 2516 K Spectral Type of Host Star: F7 V
20 Comparison of WASP 12 to an M8 Main Sequence Star Planet Mass: 1.41 M Jupiter Planet Radius: 1.79 R Jupiter Planet Temperature: 2516 K Mass: 60 M Jupiter Radius: ~1 R Jupiter Teff: ~ 2800 K 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
21 GJ 436: The First Transiting Neptune Host Star: Mass = 0.4 M סּ (M2.5 V) Butler et al. 2004
22 Special Transits: GJ 436 Butler et al Photometric transits of the planet across the star are ruled out for gas giant compositions and are also unlikely for solid compositions
23 Gillon et al The First Transiting Hot Neptune!
24 GJ 436 Star Stellar mass [ M סּ ] 0.44 ( ± 0.04) Planet Period [days] ± Eccentricity 0.16 ± 0.02 Orbital inclination Planet mass [ M E ] 22.6 ± 1.9 Planet radius [ R E ] Mean density = 1.95 gm cm 3, slightly higher than Neptune (1.64)
25 HD 17156: An eccentric orbit planet M = 3.11 M Jup Probability of a transit ~ 3%
26 Barbieri et al R = 0.96 R Jup Mean density = 4.88 g/cm 3 Mean for M2 star 4.3 g/cm 3
27 d min = 0.03 AU d max = 0.87 AU HD 80606: Long period and eccentric R = 1.03 R Jup ρ = 4.44 (cgs) a = 0.45 AU
28 MEarth-1b: A transiting Superearth D Charbonneau et al. Nature 462, (2009) doi: /nature08679
29 Change in radial velocity of GJ1214. D Charbonneau et al. Nature 462, (2009) doi: /nature08679
30 ρ = 1.87 (g/cm 3 )
31 So what do all of these transiting planets tell us? 5.5 g/cm 3 ρ = 1.25 g/cm g/cm 3 ρ = 1.24 g/cm 3 ρ = 0.62 g/cm 3
32 The density is the first indication of the internal structure of the exoplanet Solar System Object ρ (g 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 Iron Meteorites 7 8 Comets
33 Take your favorite composition and calculate the mass-radius relationship
34 Masses and radii of transiting planets. H/He dominated Pure H % H 2 0, 22% Si 67.5% Si mantle 32.5% Fe (earth-like)
35 Kepler 7b CoRoT 2b Kepler 8b CoRoT 5b Kepler 6b CoRoT 6b The The mass-radius relationship of of planets depends on on their their mass, mass, composition and and inner inner structure Cold & Hot Jupiters CoRoT 9b Hot Neptunes CoRoT 7b (Sasselov 2008) Super Earths
36 S J N
37 Sato et al HD : A planet with a large core Period = 2.87 d R p = 0.7 R Jup M p = 0.36 M Jup Mean density = 2.8 gm/cm 3
38 10-13 M earth core ~70 M earth core mass is difficult to form with gravitational instability. HD b provides strong support for the core accretion theory R p = 0.7 R Jup M p = 0.36 M Jup Mean density = 2.8 gm/cm 3
39 Planet Radius Most transiting planets tend to be inflated. Approximately 68% of all transiting planets have radii larger than 1.1 R Jup.
40 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
41 Possible Explanations for the Large Radii 2. Slight orbital eccentricity (difficult to measure) causes tidal heating of core larger radius Slight Problem: HD 17156b: e=0.68 HD 80606b: e=0.93 CoRoT 10b: e=0.53 R = 1.02 R Jup R = 0.92 R Jup R = 0.97R Jup Caveat: These planets all have masses 3-4 M Jup, so it may be the smaller radius is just due to the larger mass. 3. We do not know what is going on.
42 Density Distribution 14 S J/U N Number N Density (cgs)
43 Comparison of Mean Densities Giant Planets with M < 2 M Jup : 0.78 cgs HD 17156, P = 21 d, e= 0.68 M = 3.2 M Jup, density = 3.8 HD 80606, P = 111 d, e=0.93, M = 3.9 M Jup, density = 6.4 CoRoT 10b, P=13.2, e= 0.53, M = 2.7 M Jup, density = 3.7 CoRoT 9b, P = 95 d, e=0.12, M = 1 M Jup, density = 0.93 The three eccentric transiting planets have high mass and high densities. Formed by mergers?
44 Number Period Distribution for short period Exoplanets Period (Days) Transits RV
45 Both RV and Transit Searches show a peak in the Period at 3 days The 3 day period may mark the inner edge of the proto-planetary disk, => where migration stops?
46 Mass-Radius Relationship Kepler 11b Radius is roughly independent of mass, until you get to small planets (rocks)
47 Planet Mass Distribution RV Planets Close in planets tend to have lower mass, as we have seen before. Transiting Planets
48 Stellar Mass (solar units) 30 Host Star Mass Distribution Transiting Planets Nmber RV Planets
50 Summary of Global Properties of Transiting Planets 1. Mass Radius Diagram!!!! => internal composition 2. Transiting giant planets (close-in) tend to have inflated radii (much larger than Jupiter) 3. A significant fraction of transiting giant planets are found around early-type stars with masses 1.3 M sun. 4. The period distribution of close-in planets peaks around P 3 days. 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
51 Early indications are that the host stars of transiting planets have different properties than non-transiting planets (more details later). 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 preselected. 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
52 The Rossiter-McClaughlin Effect v v 3 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.
53 The effect was discovered in 1924 independently by Rossiter and McClaughlin Curves show Radial Velocity after removing the binary orbital motion
55 The Rossiter-McLaughlin Effect or Rotation Effect For rapidly rotating stars you can see the planet in the spectral line
56 The Rossiter-McClaughlin Effect v +v v +v 0 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. 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 positive velocities from the receeding portion of the star) you thus see a displacement to + RV.
57 The Rossiter-McClaughlin Effect What can the RM effect tell you? 1) The orbital inclination Planet a2 a a2
58 The Rossiter-McClaughlin Effect 2) The direction of the orbit Planet b
59 The Rossiter-McClaughlin Effect 2) The alignment of the orbit Planet c d
60 λ Orbital plane What can the RM effect tell you? 3. Are the spin axes aligned?
61 HD λ = 0.1 ± 2.4 deg
62 What about HD 17156? Narita et al. (2007) reported a large (62 ± 25 degree) misalignment between planet orbit and star spin axes!
63 Cochran et al. 2008: λ = 9.3 ± 9.3 degrees No misalignment!
64 Hebrard et al XO-3-b λ = 70 degrees
65 Winn et al. (2009) recent R-M measurements for X0-3 λ = 37 degrees
66 Fabricky & Winn, 2009, ApJ, 696, 1230
67 HAT-P7 λ = 182 deg!
68 HIRES data: M. Endl HARPS data : F. Bouchy Model fit: F. Pont Lambda ~ 80 deg!
69 Summary of R-M measurements: Number λ (deg) 40% of Short Period Exoplanets show significant misalignments 20% of Short Period Exoplanets are even in retrograde orbits What are the implications? Very violent past, probably due to gravitational scattering of 2 (or more) gas giant planets!
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