9
LETTER doi:10.1038/nature12767 A rocky composition for an Earth-sized exoplanet Andrew W. Howard 1 , Roberto Sanchis-Ojeda 2 , Geoffrey W. Marcy 3 , John Asher Johnson 4 , Joshua N. Winn 2 , Howard Isaacson 3 , Debra A. Fischer 5 , Benjamin J. Fulton 1 , Evan Sinukoff 1 & Jonathan J. Fortney 6 Planets with sizes between that of Earth (with radius R ) and Neptune (about 4R ) are now known to be common around Sun-like stars 1–3 . Most such planets have been discovered through the transit technique, by which the planet’s size can be determined from the fraction of star- light blocked by the planet as it passes in front of its star. Measur- ing the planet’s mass—and hence its density, which is a clue to its composition—is more difficult. Planets of size 2–4R have proved to have a wide range of densities, implying a diversity of compositions 4,5 , but these measurements did not extend to planets as small as Earth. Here we report Doppler spectroscopic measurements of the mass of the Earth-sized planet Kepler-78b, which orbits its host star every 8.5 hours (ref. 6). Given a radius of 1.20 6 0.09R and a mass of 1.69 6 0.41M , the planet’s mean density of 5.3 6 1.8 g cm 23 is similar to Earth’s, suggesting a composition of rock and iron. Kepler-78 is one of approximately 150,000 stars whose brightness was precisely measured at 30-min intervals for four years by NASA’s Kepler spacecraft 7 . This star is somewhat smaller, less massive and younger than the Sun (Table 1). Every 8.5hours the star’s brightness declines by 0.02% as the planet Kepler-78b transits (passes in front of) the stellar disk. The planet’s radius was originally measured 6 to be 1:16 z0:19 {0:14 R . Its mass could not be measured, although masses exceeding 8M could be ruled out because the planet’s gravity would have deformed the star and produced brightness variations that were not detected. We measured the mass of Kepler-78b by tracking the line-of-sight component of the host star’s motion (the radial velocity) that is due to the gravitational force of the planet. The radial-velocity analysis is challen- ging not only because the signal is expected to be small (about 1–3 m s 21 ) but also because the apparent Doppler shifts due to rotating star spots are much larger (about 50 m s 21 peak-to-peak). Nevertheless the detection proved to be possible, thanks to the precisely known orbital period and phase of Kepler-78b that cleanly separated the timescale of spot variations (P rot < 12.5 days) from the much shorter timescale of the planetary orbit (P < 8.5 hours). We adopted a strategy of intensive Doppler measurements spanning 6–8hours per night, long enough to cover nearly the entire orbit and short enough for the spot variations to be nearly frozen out. We measured radial velocities using optical spectra of Kepler-78 that we obtained from the High Resolution Echelle Spectrometer (HIRES) 8 on the 10-m Keck I Telescope. These Doppler shifts were computed relative to a template spectrum with a standard algorithm 9 that uses a spectrum of molecular iodine superposed on the stellar spectrum as a reference for the wavelength scale and instrumental profile of HIRES 1 Institute for Astronomy, University of Hawaii at Manoa, 2680 Woodlawn Drive, Honolulu, Hawaii 96822, USA. 2 Department of Physics, and Kavli Institute for Astrophysics and Space Research, Massachusetts Institute of Technology, Cambridge, Massachusetts 02139, USA. 3 Astronomy Department, University of California, Berkeley, California 94720, USA. 4 Harvard-Smithsonian Center for Astrophysics, 60 Garden Street, Cambridge, Massachusetts 02138, USA. 5 Department of Astronomy, Yale University, New Haven, Connecticut 06510, USA. 6 Department of Astronomy and Astrophysics, University of California, Santa Cruz, California 95064, USA. Table 1 | Kepler-78 system properties Stellar properties Names Kepler-78, KIC 8435766, Tycho 3147-188-1 Effective temperature, T eff 5,121 6 44 K Logarithm of surface gravity, log[g (cm s 22 )] 4.61 6 0.06 Iron abundance, [Fe/H] 20.08 6 0.04 dex Projected rotational velocity, Vsini 2.6 6 0.5 km s 21 Mass, M star 0.83 6 0.05M Sun Radius, R star 0.74 6 0.05R Sun Density, r star 2:8 z0:7 {0:6 g cm 23 Age 625 6 150 million years Planetary properties Name Kepler-78b Mass, M pl 1.69 6 0.41M Radius, R pl 1.20 6 0.09R Density, r pl 5:3 z2:0 {1:6 g cm 23 Surface gravity, g pl 11:4 z3:5 {3:1 ms 22 Iron fraction 0.20 6 0.33 (two-component rock/iron model) Orbital period, P orb (from ref. 6) 0.35500744 6 0.00000006 days Transit epoch, t c (from ref. 6) 2454953.95995 6 0.00015 (BJD TBD ) Additional parameters (R pl /R star ) 2 217 6 9 parts per million Scaled semi-major axis, a/R star 2.7 6 0.2 Doppler amplitude, K 1.66 6 0.40 m s 21 Systemic radial velocity 23.59 6 0.10 km s 21 Radial-velocity jitter, s jitter 2.1 6 0.3 m s 21 Radial-velocity dispersion 2.6 m s 21 (s.d. of residuals to best-fit model) The stellar effective temperature and iron abundance were obtained by fitting stellar atmosphere models 21 to iodine-free HIRES spectra, subject to a constraint on the surface gravity based on stellar evolution models 22 . We estimated the stellar mass and radius from empirically calibrated relationships between those spectroscopic parameters 23 . The refined stellar radius led to a refined planet radius. Planet mass and density were measured from the Doppler analysis. The stellar age is estimated from non-detection of lithium in the stellar atmosphere (Extended Data Fig. 1), the stellar rotation period, and magnetic activity. See Methods for details. Parameter distributions are represented by median values and 68.3% confidence intervals. Correlations between transit parameters are shown in Extended Data Fig. 2. Barycentric Julian dates in barycentric dynamical time, BJDTBD. 00 MONTH 2013 | VOL 000 | NATURE | 1 Macmillan Publishers Limited. All rights reserved ©2013

A rock composition_for_earth_sized_exoplanets

Embed Size (px)

DESCRIPTION

 

Citation preview

Page 1: A rock composition_for_earth_sized_exoplanets

LETTERdoi:10.1038/nature12767

A rocky composition for an Earth-sized exoplanetAndrew W. Howard1, Roberto Sanchis-Ojeda2, Geoffrey W. Marcy3, John Asher Johnson4, Joshua N. Winn2, Howard Isaacson3,Debra A. Fischer5, Benjamin J. Fulton1, Evan Sinukoff1 & Jonathan J. Fortney6

Planets with sizes between that of Earth (with radius R›) and Neptune(about 4R›) are now known to be common around Sun-like stars1–3.Most such planets have been discovered through the transit technique,by which the planet’s size can be determined from the fraction of star-light blocked by the planet as it passes in front of its star. Measur-ing the planet’s mass—and hence its density, which is a clue to itscomposition—is more difficult. Planets of size 2–4R› have proved tohave a wide range of densities, implying a diversity of compositions4,5,but these measurements did not extend to planets as small as Earth.Here we report Doppler spectroscopic measurements of the mass ofthe Earth-sized planet Kepler-78b, which orbits its host star every8.5 hours (ref. 6). Given a radius of 1.20 6 0.09R› and a mass of1.69 6 0.41M›, the planet’s mean density of 5.3 6 1.8 g cm23 issimilar to Earth’s, suggesting a composition of rock and iron.

Kepler-78 is one of approximately 150,000 stars whose brightnesswas precisely measured at 30-min intervals for four years by NASA’sKepler spacecraft7. This star is somewhat smaller, less massive andyounger than the Sun (Table 1). Every 8.5 hours the star’s brightnessdeclines by 0.02% as the planet Kepler-78b transits (passes in front of)the stellar disk. The planet’s radius was originally measured6 to be1:16z0:19

{0:14R›. Its mass could not be measured, although masses exceeding

8M› could be ruled out because the planet’s gravity would havedeformed the star and produced brightness variations that were notdetected.

We measured the mass of Kepler-78b by tracking the line-of-sightcomponent of the host star’s motion (the radial velocity) that is due tothe gravitational force of the planet. The radial-velocity analysis is challen-ging not only because the signal is expected to be small (about 1–3 m s21)but also because the apparent Doppler shifts due to rotating star spots aremuch larger (about 50 m s21 peak-to-peak). Nevertheless the detectionproved to be possible, thanks to the precisely known orbital period andphase of Kepler-78b that cleanly separated the timescale of spot variations(Prot < 12.5 days) from the much shorter timescale of the planetary orbit(P < 8.5 hours). We adopted a strategy of intensive Doppler measurementsspanning 6–8 hours per night, long enough to cover nearly the entireorbit and short enough for the spot variations to be nearly frozen out.

We measured radial velocities using optical spectra of Kepler-78 thatwe obtained from the High Resolution Echelle Spectrometer (HIRES)8

on the 10-m Keck I Telescope. These Doppler shifts were computedrelative to a template spectrum with a standard algorithm9 that uses aspectrum of molecular iodine superposed on the stellar spectrum as areference for the wavelength scale and instrumental profile of HIRES

1Institute for Astronomy, University of Hawaii at Manoa, 2680 Woodlawn Drive, Honolulu, Hawaii 96822, USA. 2Department of Physics, and Kavli Institute for Astrophysics and Space Research,Massachusetts Institute of Technology, Cambridge, Massachusetts 02139, USA. 3Astronomy Department, University of California, Berkeley, California 94720, USA. 4Harvard-Smithsonian Center forAstrophysics, 60 Garden Street, Cambridge, Massachusetts 02138, USA. 5Department of Astronomy, Yale University, New Haven, Connecticut 06510, USA. 6Department of Astronomy and Astrophysics,University of California, Santa Cruz, California 95064, USA.

Table 1 | Kepler-78 system propertiesStellar properties

Names Kepler-78, KIC 8435766, Tycho 3147-188-1Effective temperature, Teff 5,121 6 44 KLogarithm of surface gravity, log[g (cm s22)] 4.61 6 0.06Iron abundance, [Fe/H] 20.08 6 0.04 dexProjected rotational velocity, Vsini 2.6 6 0.5 km s21

Mass, Mstar 0.83 6 0.05MSun

Radius, Rstar 0.74 6 0.05RSun

Density, rstar 2:8z0:7{0:6 g cm23

Age 625 6 150 million years

Planetary properties

Name Kepler-78bMass, Mpl 1.69 6 0.41M›

Radius, Rpl 1.20 6 0.09R›

Density, rpl 5:3z2:0{1:6 g cm23

Surface gravity, gpl 11:4z3:5{3:1 m s22

Iron fraction 0.20 6 0.33 (two-component rock/iron model)Orbital period, Porb (from ref. 6) 0.35500744 6 0.00000006 daysTransit epoch, tc (from ref. 6) 2454953.95995 6 0.00015 (BJDTBD)

Additional parameters

(Rpl/Rstar)2 217 6 9 parts per million

Scaled semi-major axis, a/Rstar 2.7 6 0.2Doppler amplitude, K 1.66 6 0.40 m s21

Systemic radial velocity 23.59 6 0.10 km s21

Radial-velocity jitter, sjitter 2.1 6 0.3 m s21

Radial-velocity dispersion 2.6 m s21 (s.d. of residuals to best-fit model)

The stellar effective temperature and iron abundance were obtained by fitting stellar atmosphere models21 to iodine-free HIRES spectra, subject to a constraint on the surface gravity based on stellar evolutionmodels22. We estimated the stellar mass and radius from empirically calibrated relationships between those spectroscopic parameters23. The refined stellar radius led to a refined planet radius. Planet mass anddensity were measured from the Doppler analysis. The stellar age is estimated from non-detection of lithium in the stellar atmosphere (Extended Data Fig. 1), the stellar rotation period, and magnetic activity. SeeMethods for details. Parameter distributionsare representedby median values and 68.3% confidence intervals. Correlations between transit parameters are shown in Extended Data Fig. 2. Barycentric Julian datesin barycentric dynamical time, BJDTBD.

0 0 M O N T H 2 0 1 3 | V O L 0 0 0 | N A T U R E | 1

Macmillan Publishers Limited. All rights reserved©2013

Page 2: A rock composition_for_earth_sized_exoplanets

(Supplementary Table 1). Exposures lasted 15–30 min depending on con-ditions and produced radial velocities with 1.5–2.0 m s21 uncertainties.The time series of radial velocities spans 45 days, with large velocity offsetsbetween nights due to star spots (Fig. 1). Within each night the radial velo-cities vary by typically 2–4 m s21 and show coherence on shorter timescales.

We modelled the radial-velocity time series as the sum of two com-ponents. One component was a sinusoidal function representing orbitalmotion (assumed to be circular). The orbital period and phase were heldfixed at the photometrically determined values; the only free parameterswere the Doppler amplitude K, an arbitrary radial-velocity zero point,and a velocity ‘jitter’ term sjitter to account for additional radial-velocitynoise. The second component of the model, representing the spot varia-tions, was the sum of three sinusoidal functions with periods Prot, Prot/2,and Prot/3. The amplitudes and phases of the sinusoids and Prot werefree parameters. All together there were ten parameters and 77 datapoints. Using a Markov Chain Monte Carlo (MCMC) method tosample the allowed combinations of the model parameters, we foundK 5 1.66 6 0.40 m s21, corresponding to Mpl 5 1.69 6 0.41M› (Fig. 1).This planet mass is consistent with an independent measurement usingthe HARPS-N spectrometer10.

Several tests were performed to gauge the robustness of the spot model.First, we varied the number of harmonics, checking at each stage whetherany improvement in the fit was statistically significant. The three-termmodel was found to provide noticeable improvement over one-termand two-term models, but additional harmonics beyond Prot/3 did notprovide significant improvement. Second, we used a different spot modelin which the spot-induced variation was taken to be a linear function oftime specific to each night. The constant and slope of each nightly functionwere free parameters. With this model we found Mpl 5 1.50 6 0.44M›,consistent with the preceding results (see Methods and Extended DataFig. 3). The larger uncertainty can be attributed to the greater flexibilityof this piecewise-linear spot model, which permits discontinuous andprobably unphysical variations between consecutive nights.

Kepler-78b is now the smallest exoplanet for which both the massand radius are known accurately (Fig. 2), extending the domain of suchmeasurements into the neighbourhood of Earth and Venus. Kepler-78bis 20% larger than Earth and is 69% more massive, suggesting com-monality with the other low-mass planets (4–8M›) below the rockcomposition contour in Fig. 2b. They are all consistent with rock/ironcompositions and negligible atmospheres.

50 60 70 80 90

Time (JD − 2,456,400)

–30

–20

–10

0

10

20

30

40

Rad

ial velo

city (m

s–1)

1 23

4

5

6 7 8

Night 1

0.70 0.95 1.20

JD − 2,456,448

–10

–5

0

5

Night 2

0.70 0.95 1.20

JD − 2,456,472

–10

–5

0

5

Night 3

0.70 0.95 1.20

JD − 2,456,473

–10

–5

0

5Night 4

0.70 0.95 1.20

JD − 2,456,475

15

20

25

30

Night 5

0.70 0.95 1.20

JD − 2,456,478

–20

–15

–10

–5

Night 6

0.70 0.95 1.20

JD − 2,456,483

–10

–5

0

5

Night 7

0.70 0.95 1.20

JD − 2,456,485

–10

–5

0

5

Night 8

0.70 0.95 1.20

JD − 2,456,486

–10

–5

0

5

0.0 0.2 0.4 0.6 0.8 1.0

Orbital phase

–5

0

5

Sp

ot-

co

rrecte

d r

ad

ial velo

city

(m s

–1)

0.0 0.2 0.4 0.6 0.8 1.0

Orbital phase

–2

–1

0

1

2

a

b

Rad

ial velo

city (m

s–1)

c d e

f g h i

j k

Figure 1 | Apparent radial-velocity variations of Kepler-78. a, The 38-daytime series of relative radial velocities (black filled circles) from Keck-HIRESalong with the best-fitting model (red line), with short-term variationsdue to orbital motion and long-term variations due to rotating star spots. Blueboxes identify the eight nights when high-cadence measurements wereundertaken. JD, Julian day. b–i, For each individual night, the measured radialvelocities (black filled circles), the spot 1 planet model (solid red lines) and spotmodel alone (dashed red lines) are shown. j, k, The phase-folded radial

velocities after subtracting the best-fitting spot model (j), and after binning inorbital phase and computing the mean radial velocities and s.e.m. for error bars(k). Planetary transits occur at zero orbital phase and solid red lines markthe phased planet model (in j and k). Each radial-velocity error bar in panelsa–j represents the s.e.m. for the Doppler shifts of around 700 segments of aparticular spectrum; it does not account for additional uncorrectedradial-velocity ‘jitter’ from astrophysical and instrumental sources.

RESEARCH LETTER

2 | N A T U R E | V O L 0 0 0 | 0 0 M O N T H 2 0 1 3

Macmillan Publishers Limited. All rights reserved©2013

Page 3: A rock composition_for_earth_sized_exoplanets

We explored some possibilities for the interior structure of Kepler-78b using a simplified two-component model11 consisting of an ironcore surrounded by a silicate mantle (Mg2SiO4). This model correctlyreproduces the masses of Earth and Venus given their radii and assum-ing a composition of 67% silicate rock and 33% iron by mass. Appliedto Kepler-78b, the model gives an iron fraction of 20% 6 33%, similarto that of Earth and Venus but smaller than that of Mercury (approxi-mately 60%; ref. 12).

With a star–planet separation of 0.01 astronomical units (1 AU is theEarth-to-Sun distance), the dayside of Kepler-78b is heated to a tem-perature of 2,300–3,100 K. Any gaseous atmosphere around Kepler-78b would probably have been lost long ago to photoevaporation bythe intense starlight13. However, based on the measured surface gravityof 11 m s22, the liquid and solid portions of the planet should be stableagainst mass loss of the sort14 that is apparently destroying the smallerplanet KIC 12557548b (ref. 15).

Kepler-78b is a member of an emerging class of planets with orbitalperiods of less than half a day6,16,17. Another member is KOI 1843.03(refs 18 and 19), which has been shown to have a high density (morethan about 7 g cm23), although the deduction in that case was based ona theoretical requirement to avoid tidal destruction rather than directmeasurement. That planet’s minimum density is similar to our estimateddensity for Kepler-78b (which is 5:3z2:0

{1:6 g cm23). These two planetsprovide a stark contrast to Kepler-11f, which has a similar mass toKepler-78b, but a density that is ten times smaller20.

With only a handful of low-mass planets with measured densitiesknown (Fig. 2b), we see solid planets primarily in highly irradiated,close-in orbits and low-density planets swollen by thick atmospheresin somewhat cooler orbits. Measurements of additional planet massesand radii are needed to assess the significance of this pattern. Additionalultrashort-period planets with detectable Doppler amplitudes (K / P21/3)have been identified by the Kepler mission and are ready for mass mea-surements. With an ensemble of future measurements, the masses andradii of ultrashort-period planets may reveal a commonality or diversityof density and composition. This knowledge of hot solid planets may

be relevant to understanding the interiors of cooler extrasolar planetswith atmospheres, establishing the range of core sizes in giant planetformation, and explaining Mercury’s unusually high iron abundance.

METHODS SUMMARYWe fitted Keck-HIRES spectra of Kepler-78 with stellar atmosphere models usingSpectroscopy Made Easy to measure the star’s temperature, gravity and iron abun-dance. These spectroscopic parameters were used to estimate the host star’s mass,radius and density—crucial parameters from which to determine the planet’s mass,radius and density—from empirical relationships calibrated by precisely charac-terized binary star systems. Using this stellar density as a constraint, we reanalysedthe Kepler photometry to refine the planet radius measurement. We observedKepler-78 with HIRES using standard procedures including sky spectrum subtrac-tion and wavelength calibration with a reference iodine spectrum. We measuredhigh-precision relative radial velocities using a forward model where the de-convolvedstellar spectrum is Doppler-shifted, multiplied by the normalized high-resolutioniodine transmission spectrum, convolved with an instrumental profile, and matchedto the observed spectra using a Levenberg–Marquardt algorithm that minimizesthe x2 statistic. The time-series radial velocities on eight nights were analysed withseveral parametric models to account for the small-amplitude, periodic signal fromthe orbiting planet and the larger-amplitude, quasi-periodic apparent Doppler shiftsthat are due to rotating starspots. In our adopted harmonic spot model the star-spotsignal was modelled as a sum of sine functions whose amplitudes and phases werefree parameters. We sampled the multi-dimensional model parameter space withan MCMC algorithm to estimate parameter confidence intervals and to accountfor covariance between parameters. We found multiple families of models thatdescribed the data well and they gave consistent measures of the Doppler ampli-tude, which is proportional to the mass of Kepler-78b.

Online Content Any additional Methods, Extended Data display items and SourceData are available in the online version of the paper; references unique to thesesections appear only in the online paper.

Received 25 September; accepted 11 October 2013.

Published online 30 October 2013.

1. Howard, A. W. et al. Planet occurrence within 0.25 AU of solar-type stars fromKepler. Astrophys. J. 201 (Suppl.), 15 (2012).

0.1 1 10 100 1,000 1 2 3 4 5 6 7 8 9 10

Planet mass (M⊕)

20

15

10

5

0

Pla

net

rad

ius (R⊕)

2.5

2.0

1.5

1.0

Hyd

rogen

Water

Rock

Iron

Wat

er

Rock

Iron

Earth-like

Mercury-like

a b

Figure 2 | Masses and radii of well-characterized planets. Extrasolar planetsare denoted by red circles and Solar System planets are represented by greentriangles. a spans the full range of sizes and masses on logarithmic axes. Theshaded grey rectangle denotes the range of parameters shown in b on linearmass and radius axes. Kepler-78b is depicted as a black filled circle in a andas a distribution of allowed masses and radii with a dotted red ellipse markingthe 68% confidence region in b. Model mass–radius relationships11,24 for

idealized planets consisting of pure hydrogen, water, rock (Mg2SiO4), and ironare shown as blue lines. Green and brown lines denote Earth-like composition(67% rock, 33% iron) and Mercury-like composition (40% rock, 60% iron).Exoplanet masses, radii and their associated errors are from the ExoplanetOrbit Database25 (http://exoplanets.org; downloaded on 1 September 2013).Planets with fractional mass uncertainties of over 50% are not shown.

LETTER RESEARCH

0 0 M O N T H 2 0 1 3 | V O L 0 0 0 | N A T U R E | 3

Macmillan Publishers Limited. All rights reserved©2013

Page 4: A rock composition_for_earth_sized_exoplanets

2. Petigura, E., Marcy, G. W. & Howard, A. A plateau in the planet population belowtwice the size of Earth. Astrophys. J. 770, 69 (2013).

3. Fressin, F. et al. The false positive rate of Kepler and the occurrence of planets.Astrophys. J. 766, 81 (2013).

4. Valencia, D., Guillot, T., Parmentier, V. & Freedman, R. S. Bulk composition of GJ1214b and other sub-Neptune exoplanets. Astrophys. J. 775, 10 (2013).

5. Fortney, J. J. et al. A framework for characterizing the atmospheres of low-masslow-density transiting planets. Astrophys. J. 775, 80 (2013).

6. Sanchis-Ojeda, R. et al. Transits and occultations of an Earth-sized planet in an8.5-hour orbit. Astrophys. J. 774, 54 (2013).

7. Borucki, W. J. et al. Kepler planet-detection mission: introduction and first results.Science 327, 977–980 (2010).

8. Vogt, S. et al. HIRES: the high-resolution echelle spectrometer on the Keck 10-mtelescope. Proc. SPIE 2198, 362–375 (1994).

9. Butler, R. P. Attaining Doppler precision of 3m s21. Publ. Astron. Soc. Pacif. 108,500–509 (1996).

10. Pepe, F. et al. An Earth-sized planet with an Earth-like density. Naturehttp://dx.doi.org/10.1038/nature12768 (this issue).

11. Fortney, J. J. et al. Planetary radii across five orders of magnitude in mass andstellar insolation: application to transits. Astrophys. J. 659, 1661–1672 (2007).

12. Hauck, S. A. IIet al. The curious caseofMercury’s internal structure. J.Geophys. Res.118, 1204–1220 (2013).

13. Lopez, E. D., Fortney, J. J. & Miller, N. How thermal evolution and mass-loss sculptpopulations of super-Earths and sub-Neptunes: application to the Kepler-11system and beyond. Astrophys. J. 761, 59 (2012).

14. Perez-Becker, D. & Chiang, E. Catastrophic evaporation of rocky planets. Mon. Not.R. Astron. Soc. 433, 2294–2309 (2013).

15. Rappaport, S. et al. Possible disintegrating short-period super-Mercury orbitingKIC 12557548. Astrophys. J. 752, 1 (2012).

16. Jackson, B., Stark, C. C., Adams, E. R., Chambers, J. & Deming, D. A survey for veryshort-period planets in the Kepler data. Astrophys. J. (submitted); preprint athttp://arxiv.org/abs/1308.1379 (2013).

17. Muirhead, P. S. et al. Characterizing the cool KOIs. III. KOI 961: a small star withlarge proper motion and three small planets. Astrophys. J. 747, 144 (2012).

18. Ofir, A. & Dreizler, S. An independent planet search in the Kepler dataset. I. Onehundred new candidates and revised Kepler objects of interest. Astron. Astrophys.555, A58 (2013).

19. Rappaport, S. et al. The Roche limit for close-orbiting planets: minimum density,composition, and application to the 4.2 hr planet KOI 1843.01. Astrophys. J. 773,L15 (2013).

20. Lissauer, J. J. et al. All six planets known to orbit Kepler-11 have low densities.Astrophys. J. 770, 131 (2013).

21. Valenti, J. A. & Fischer, D. A. Spectroscopic properties of cool stars (SPOCS). I. 1040F, G, and K dwarfs from Keck, Lick, and AAT planet search programs. Astrophys. J.159 (Suppl.), 141–166 (2005).

22. Dotter, A.et al. TheDartmouth stellar evolution database. Astrophys. J. 178 (Suppl.),89–101 (2008).

23. Torres, G., Andersen, J. & Gimenez, A. Accurate masses and radii of normal stars:modern results and applications. Astron. Astrophys. Rev. 18, 67–126 (2010).

24. Seager, S. et al. Mass-radius relationships for solid exoplanets. Astrophys. J. 669,1279–1297 (2007).

25. Wright, J. T. et al. The exoplanet orbit database. Publ. Astron. Soc. Pacif. 123,412–422 (2011).

Supplementary Information is available in the online version of the paper.

Acknowledgements This Letter and another10 were submitted simultaneously and arethe result of coordinated, independent radial-velocity observations and analyses ofKepler-78. We thank the HARPS-N team for their collegiality. We also thank E. Chiang,I. Crossfield, R. Kolbl, E. Petigura, and D. Huber for discussions, S. Howard for support,C. Dressing for a convenient packaging of stellar models, and A. Hatzes for a thoroughreview. This work was based on observations at the W. M. Keck Observatory granted bythe University of Hawaii, the University of California, and the California Institute ofTechnology. We thank the observers who contributed to the measurements reportedhere and acknowledge the efforts of the Keck Observatory staff. We thank those ofHawaiian ancestry on whose sacred mountain of Mauna Kea we are guests. Kepler wascompetitively selected as the tenth Discovery mission with funding providedbyNASA’sScience Mission Directorate. J.N.W. and R.S.-O. acknowledge support from the KeplerParticipating Scientist programme. A.W.H. acknowledges funding from NASA grantNNX12AJ23G.

Author Contributions This measurement was conceived and planned by A.W.H.,G.W.M., J.A.J., J.N.W. and R.S.-O. HIRES observations were conducted by A.W.H., G.W.M.,H.I, B.J.F. and E.S. The HIRES spectra were reduced and Doppler-analysed by A.W.H.,G.W.M., H.I. and J.A.J. Data modelling was done primarily by A.W.H. and R.S.-O. A.W.H.was the primary author of the manuscript, with important contributions from J.N.W.,R.S.-O. and J.J.F. Figures were generated by A.W.H., R.S.-O, B.J.F. and E.S. All authorsdiscussed the results, commented on the manuscript and contributed to theinterpretation.

Author Information Reprints and permissions information is available atwww.nature.com/reprints. The authors declare no competing financial interests.Readers are welcome to comment on the online version of the paper. Correspondenceand requests for materials should be addressed to A.W.H. ([email protected]) orR.S.-O. ([email protected]).

RESEARCH LETTER

4 | N A T U R E | V O L 0 0 0 | 0 0 M O N T H 2 0 1 3

Macmillan Publishers Limited. All rights reserved©2013

Page 5: A rock composition_for_earth_sized_exoplanets

METHODSStellar characterization. We fitted three Keck-HIRES spectra of Kepler-78 withstellar atmosphere models using Spectroscopy Made Easy (SME26). The spectrahave per-pixel signal-to-noise ratios of 220 at 550 nm. We used the standard wave-length intervals, line data and methodology21. Kepler-78 does not have a measuredparallax with which to constrain luminosity and gravity. The initial analysis gavean effective temperature Teff 5 5,119 6 44 K, a gravity value of log[g (cm s22)] 5

4.751 6 0.060, an iron abundance of [Fe/H] 5 20.054 6 0.040 dex, and a pro-jected rotational velocity of Vsini 5 2.2 6 0.5 km s21. These values are the mean ofthe SME results for the three spectra and the error bars are limited by systematics21.Because this combination of Teff and log(g) is inconsistent with the Dartmouthstellar evolutionary model22, we recomputed stellar parameters with log(g) fixed atthe value that is predicted by a stellar model at the value of Teff from SME, resultingin the stellar parameters in Table 1. We note that the adopted Vsini 5 2.6 6 0.5 km s-1

is consistent with an expectation based on a stellar rotation, size and an equatorialviewing geometry: Vsini < Vrot < 2pRstar/Prot 5 3.0 km s21.

We estimated the stellar mass and radius using empirical relationships23 basedon non-interacting binary systems that parameterize Rstar and Mstar as functions oflog(g), Teff and [Fe/H]. We propagated the errors on the three SME-derived inputsto obtain Rstar 5 0.74 6 0.05RSun and Mstar 5 0.83 6 0.05MSun. The Mstar uncer-tainty comes from the 6% fractional scatter in the mass–radius relationship23. Weadopt these values when computing Rpl and Mpl. We checked for self-consistencyof the empirical calibration by computing log(g) from the derived Rstar and Mstar,giving log[g (cm s22)] 5 4.62 6 0.06.

As a consistency check, we explored two additional estimates of stellar para-meters. First, the mass and radius from an evolutionary track in the Dartmouthmodel (one billion years, metal abundance [m/H] 5 0) that match our adopted Teff

and log(g) values are Rstar 5 0.77 6 0.04RSun and Mstar 5 0.85 6 0.05MSun. Thesevalues are consistent with our adopted results. Second, we used a recent study27 ofstellar angular diameters that parameterized Rstar as a function of Teff. This givesRstar 5 0.77 6 0.03RSun, where the uncertainty is the median absolute deviation onthe calibration star radii.

We note that Kepler-78 has remarkably similar properties to the transiting planethost star HD 189733. These properties28,29 include Teff 5 5,040 K, log[g (cm s22)] 5

4.587, Rstar 5 0.76RSun and Mstar 5 0.81MSun, stellar activity index log(R0HK ) 5 24.50,and Prot 5 11.9 days. HD 189733 has spot-induced radial-velocity variations30 of,15 m s21 (rms).

The rotation period of Kepler-78 was previously measured to be 12.5 6 1.0 days6.Using a relationship31 between age, mass and rotation period, we estimate its age tobe 750 6 150 million years. The stellar age can also be estimated from the stellarmagnetic activity measured by the SHK index. We computed the spectral-type-independent activity index, log(R0HK ), for all HIRES observations of this star andfound a median value of 24.52 with a 1s range of 60.03. The computation madeuse of an estimated broadband photometric colour B 2 V 5 0.873, converted21

from Teff. This level of activity is consistent with the value for stars in the 625-million-year-old Hyades cluster31. We also constrained the age by searching for theage-sensitive Li I absorption line at 6,708 A. Lithium is depleted relatively quicklyin stars of this spectral type by convective mixing. Based on Li I measurements inthree clusters with known ages32, our non-detection (Extended Data Fig. 1) suggestsan age greater than around 500 million years. These three ages are self-consistent.We adopt an age of 625 million years with an approximate age uncertainty of150 million years. We expect a star of this age and activity to have spots that causeradial-velocity variations at the .10 m s21 level.Transit analysis. Transit parameters are crucial to estimating the planet radius,which in turn affects our ability to estimate the composition of the planet. Theseparameters were measured previously with the discovery of Kepler-78b (ref. 6). Inthat study the impact parameter b was nearly unconstrained because the 30-mintime sampling of the Kepler long-cadence data cannot resolve the transit ingresstime. This leads to an increased uncertainty on transit depth owing to the stellarlimb-darkening profile. We constrained the transit parameters using the stellardensity (rstar) obtained from the spectroscopic analysis. Assuming a circular orbit:

rstar~(3p=GP2) a=Rstarð Þ3

where a/Rstar is the scaled semi-major axis, G is the gravitational constant, and P isthe orbital period33. This gives a/Rstar 5 2.7 6 0.2, a much tighter constraint thanfrom the transit light curve alone (a/Rstar 5 3:0z0:5

{1:0).Aside from this additional constraint, our transit analysis is similar to the one in

ref. 6. In brief, we analysed the Kepler long-cadence data from quarters 1–15 (atotal of 3.7 years of nearly continuous observations) to construct a filtered, phase-folded light curve with a final cadence of 2 min. The light curve is modelled with acombination of a transit model34, a model for the out-of-transit modulations andan occultation model. The most relevant transit parameters are the impact parameter,

the ratio of stellar radius to orbital distance, and the zero-limb-darkening transitdepth. The model is calculated with a cadence of 15 s and averaged over the 30-mincadence of Kepler. In this new analysis, a/Rstar is subjected to a Gaussian prior(2.7 6 0.2), which leads to a well-measured impact parameter and a reduced uncer-tainty for the transit depth. We found the best-fit solution and explored parameterspace using an MCMC algorithm. The final parameters are (Rpl/Rstar)

2 5 217z9{10

parts per million, impact parameter b 5 0:68z0:05{0:02, orbital inclination i 5 75:2z2:6

{2:1deg,a transit duration of 0.813 6 0.014 hours, and Rpl 5 1.20 6 0.09R›. Error barsencompass 68.3% confidence intervals. Parameter correlations are plotted inExtended Data Fig. 2. These values are compatible with the previous estimate thatwas not constrained by rstar (ref. 6).Radial-velocity measurements. We observed Kepler-78 with the HIRES echellespectrometer8 on the 10-m Keck I telescope using standard procedures. Observa-tions were made with the C2 decker (a rectangular opening in the HIRES entrance)(14 3 0.86 arcsec). This slit is long enough to simultaneously record spectra ofKepler-78 and the faint night sky. We subtracted the sky spectra from the spectraof Kepler-78 during the spectral reduction35.

Light from the telescope passed through a glass cell of molecular iodine heated to50 uC. The dense set of molecular absorption lines imprinted on the stellar spectrafrom 5,000 A to 6,200 A provide a robust wavelength scale against which Dopplershifts are measured, as well as strong constraints on the instrumental profile at thetime of each observation36,37. We also obtained three iodine-free ‘template’ spectraof Kepler-78 using the B3 decker (14 3 0.57 arcsec). These spectra were used tomeasure stellar parameters, as described above. One of them was de-convolvedusing the instrumental profile measured from spectra of rapidly rotating B starsobserved immediately before and after. This de-convolved spectrum served as a‘template’ for the Doppler analysis.

The HIRES observations span 45 days. On eight nights we observed Kepler-78intensively, covering 6–8 hours per night. We also gathered a single spectrum onsix additional nights to monitor the radial-velocity variations from spots. Theseonce-per-night radial velocities were not used to determine the planetary mass andare shown in Extended Data Fig. 3 but not in Fig. 1.

We measured high-precision relative radial velocities using a forward modelwhere the de-convolved stellar spectrum is Doppler-shifted, multiplied by the norma-lized high-resolution iodine transmission spectrum, convolved with an instrumentalprofile, and matched to the observed spectra using a Levenberg–Marquardt algorithmthat minimizes the x2 statistic9. In this algorithm, the radial velocity is varied (alongwith nuisance parameters describing the wavelength scale and instrumental profile)until the x2 minimum is reached.

The times of observation (in heliocentric Julian days, HJD), radial velocitiesrelative to an arbitrary zero point, and error estimates are listed in SupplementaryTable 1 and plotted in Extended Data Fig. 3. Each radial-velocity error is the standarderror on the mean radial velocity of about 700 spectral chunks (each spanning about2 A) that are separately Doppler-analysed. These error estimates do not account forsystematic Doppler shifts from instrumental or stellar effects. We also measuredthe SHK index for each HIRES spectrum. This index measures the strength of theinversion cores of the Ca II H and K absorption lines and correlates with stellarmagnetic activity38.

We measured the absolute radial velocity of Kepler-78 relative to the Solar Systembarycentre using telluric sky lines as a reference39. The distribution of telluric radialvelocities has a median value of 23.59 km s21 and a standard deviation of 0.10 km s21.Harmonic radial-velocity spot model. Kepler-78 is a young active star, as demon-strated by the large stellar flux variations observed with Kepler. A previous study6

measured Prot 5 12.5 6 1.0 days using a Lomb–Scargle periodogram of the pho-tometry. Inspection of the radial velocities measured over one month do indeedshow some repeatability with a timescale of about 12–13 days, a sign that star spotsare also inducing a large radial-velocity signal (see Extended Data Fig. 3). Usingprevious work40, we modelled the radial-velocity signal induced by spots with aprimary sine function at the rotation period of the star, followed by a series of sinefunctions representing the harmonics of the stellar rotation frequency. The planet-induced radial-velocity signal is modelled with a sinusoid, assuming zero eccent-ricity and using a linear ephemeris fixed to the best-fit orbital period and phase6.The final model for the radial velocity at time t is:

RV tð Þ~{Ksin 2p t{tcð Þ=P½ �zczX

i

aisin Qizi2pt=Prot½ �

where K is the semi-amplitude of the planet-induced radial-velocity signal, tc is atime of transit, P is the orbital period, c is an arbitrary radial velocity offset, i runsfrom 1 to N, where N is the number of harmonics used, Prot is the rotation period,and finally ai and Qi are the two parameters added for each of the N harmonics. Theamplitude ai is always chosen to be positive, and Qi is constrained to be positive andsmaller than 2p. The time t was set to zero at 2,456,446 in HJD format. P and tc were

LETTER RESEARCH

Macmillan Publishers Limited. All rights reserved©2013

Page 6: A rock composition_for_earth_sized_exoplanets

held fixed to their photometrically determined values (Table 1). K was free to takeon positive and negative values to prevent a bias towards larger planet mass.

We used the Bayesian Information Criterion to choose the appropriate numberof harmonics. This criterion states that for each additional model parameter thestandard x2 function should decrease by at least ln(Nmeas) to be deemed statisticallysignificant. In our case Nmeas 5 77 (the number of radial velocities on the eightnights with intensive observations). For each harmonic added, the best-fit x2

should decrease by at least 8.7 for the more complex model to be justified. Thebest-fit x2 values for N 5 1, 2, 3, 4 and 5 were 1,822, 262, 163, 161 and 158,respectively. We used a Gaussian distribution as a prior on the rotation periodin this analysis to select the number of harmonics. We adopted the N 5 3 modelbecause adding additional harmonics is not statistically justified.

This analysis does not rule out the possibility that non-consecutive harmonicsprovide a better fit to the data. We checked that for a model with three harmonicschosen from the first four, the first three harmonics is the best combination. Wealso checked that choosing only two harmonics out of the first four was never abetter option than using the first three.

Using the spot model with the first three harmonics, we used an MCMCalgorithm to explore the model parameter space. We added a radial-velocity ‘jitter’term sjitter to account for the high value of the reduced x2 in the best-fit modelwithout jitter (a value of 2.1), following a standard procedure41 to leave it as a freeparameter. We maximized the logarithm of the likelihood function instead ofminimizing the x2 function. We estimate the parameters describing the planet to beK51.666 0.40 m s21, c54:4z2:7

{2:0 m s21, and sjitter 52:08z0:32{0:29 m s21. The para-

meters descripting the starspots are Prot 5 12.78 6 0.04 days, a1 53:6z3:6{1:4 m s21,

a2510:5z3:3{2:4 ms21,a3510:2z1:5

{1:3 ms21,Q154:4z1:2{1:0,Q253:9z0:2

{0:3 andQ350.4860.21.These values are the median and 68.3% confidence regions of marginalizedposterior distributions from the MCMC analysis. In this final run, Prot was notsubject to a prior and yet the value is compatible with the photometric estimate.Our estimate of K is inconsistent with zero at the 4s level. This 4s detection ofKepler-78b that is consistent with the orbital period and phase from Kepler givesus high confidence that we have detected the planet. The planet mass listed inTable 1 was computed from the values for K, P, i and Mstar with the assumption ofa circular orbit.

We searched for additional x2 minima to assess the sensitivity of our massmeasurement to the spot model. We found a second family of solutions withK 5 1.85 6 0.43 m s21, sjitter 5 2.3 6 0.3 m s21, and Prot 5 12.3 days. Althoughour adopted solution with Prot 5 12.8 days is clearly preferred by the x2 criterion(x2 5 163 versus 180), the broader model search demonstrates that our massdetermination is relatively insensitive to details of the spot model.

We also calculated the K values with different combinations of two and threeharmonics. For example, a model with the first, second and fourth harmonic givesK 5 1.78 6 0.45 m s21, with a slightly larger sjitter 5 2.3 6 0.3 m s21. A model withthe first four harmonics gives K 5 1.77 6 0.41 m s21, with sjitter 5 2.2 6 0.3 m s21.Second, we included all of the radial velocities (including the six radial velocitiesmeasured on nights without intensive observations) and fitted the complete dataset with three and four consecutive harmonics, giving K 5 1.80 6 0.43 m s21 andsjitter 5 2.4 6 0.3 m s21 for the three-harmonics model, and K 5 1.77 6 0.41 m s21

and sjitter 5 2.2 6 0.3 m s21 for the four-harmonics model. Although the coeffi-cients and phases of the sine functions changed with each test, K remained com-patible with the value from our adopted model. We also checked that K is notcorrelated with any other model parameters in the MCMC distribution.

We estimate the probability that radial-velocity noise fluctuations conspired toproduce an apparently coherent signal with the precise period and phase of Kepler-78b to be approximately one in 16,000. This is the probability of a 4s outlier for anormally distributed random variable. We adopt 4s because the fractional error onK is approximately 4. Note that this is not the false alarm probability commonlycomputed for new Doppler detections of exoplanets. In those cases one mustsearch over a wide range of orbital periods and phases to detect the planet, andalso measure the planet’s mass. Here the existence of the planet was already wellestablished6. Our task was to measure the planet’s mass given knowledge of its orbit.Offset-slope radial-velocity spot model. To gauge the sensitivity of our results tomodel assumptions, we considered a second radial-velocity model. Like the harmonicspot model, the offset-slope model consists of two components. The Doppler signalfrom the planet is a sinusoidal function of time with the period and phase held fixedat the values from the photometric analysis. The spot variations are approximated

as linear functions of time with slopes and offsets specific to each night, providingmuch greater model flexibility42. This model for the radial velocity at time t onnight n is:

RV tð Þ~{Ksin 2p t{tcð Þ=P½ �zcnz_cn t{tnð Þwhere cn is a radial-velocity offset, _cn is a radial-velocity slope (velocity per unit

time), and tn is the median time of observation specific to night n. The othersymbols are as defined above. As with the previous model, a radial-velocity jitterterm was added in quadrature to the errors and P and tc were fixed (Table 1). Alltogether, the offset-slope model contains 18 free parameters.

We used an MCMC algorithm to explore the model parameter space. The best-fit model and randomly selected models from the MCMC chain are shown inExtended Data Fig. 3. The key result is K 5 1.53 6 0.45 m s21, which is consistentwith the value from the harmonic spot model. The lower precision of the offset-slope model (3.4s versus 4.1s significance) results from greater model flexibility.The slopes and offsets on nearby nights are not constrained to produce continuousspot variations as a function of time. For this reason we adopted the harmonic spotmodel.

As an additional test of the sensitivity to model details, we used the offset-slopeframework to model a subset of the radial velocities. Within each night, we selectedthe median values from each group of three radial velocities ordered in time. Thisselection naturally rejects outlier radial velocities and matches the observing styleon nights 2–8 when three groups of three measurements were made as close aspossible to orbital quadratures (maximum or minimum radial velocity). (On night8, the final group of radial velocities has only two measurements; we used the meanof those two radial velocities for this test.) Our MCMC analysis of these medianradial velocities gave a similar result, K 5 1.26 6 0.38 m s21, that is consistent withthe above results at about the 1s level. We conclude that our detection of Kepler-78is not strongly sensitive to spot model assumptions or to individual radial-velocitymeasurements.

26. Valenti, J. & Piskunov, N. Spectroscopy made easy: a new tool for fittingobservations with synthetic spectra. Astron. Astrophys. 118 (Suppl.), 595–603(1996).

27. Boyajian, T. S. et al. Stellar diameters and temperatures. II. Main-sequence K- andM-stars. Astrophys. J. 757, 112 (2012).

28. Torres, G., Winn, J. N. & Holman, M. J. Improved parameters for extrasolartransiting planets. Astrophys. J. 667, 1324 (2012).

29. Henry, G. W. & Winn, J. N. The rotation period of the planet-hosting star HD189733. Astron. J. 135, 68–71 (2008).

30. Bouchy, F. et al. ELODIE metallicity-biased search for transiting hot Jupiters II. Avery hot Jupiter transiting the bright K star HD 189733. Astron. Astrophys. 444,L15–L19 (2005).

31. Mamajek, E. E. & Hillenbrand, L. A. Improved age estimation for solar-type dwarfsusing activity-rotation diagnostics. Astrophys. J. 687, 1264–1293 (2008).

32. Jones, B. F., Fischer, D. & Shetrone, M. The evolution of the lithium abundances ofsolar-type stars. VII. M34 (MGC 1039) and the role of rotation in lithium depletion.Astron. J. 114, 352–362 (1997).

33. Seager, S. & Mallen-Ornelas, G. A unique solution of planet and star parametersfrom an extrasolar planet transit light curve. Astrophys. J. 585, 1038–1055 (2003).

34. Mandel, K. & Agol, E. Analytic light curves for planetary transit searches. Astrophys.J. 580, L171–L175 (2002).

35. Batalha, N. et al. Kepler’s first rocky planet: Kepler-10b. Astrophys. J. 729, 27(2011).

36. Marcy, G.W. & Butler, R. P. Precision radial velocities with an iodine absorption cell.Publ. Astron. Soc. Pacif. 104, 270–277 (1992).

37. Valenti, J. A., Butler, R. P. & Marcy, G. W. 1995, Determining spectrometerinstrumental profiles using FTS reference spectra. Publ. Astron. Soc. Pacif. 107,966–976 (1995).

38. Isaacson, H. & Fischer, D. Chromospheric activity and jitter measurements for2630 stars on the California planet search. Astrophys. J. 725, 875–885 (2010).

39. Chubak, C. et al. Precise radial velocities of 2046 nearby FGKM stars and 131standards. Astrophys. J. (submitted); available at http://arxiv.org/abs/1207.6212(2012).

40. Dumusque, X. et al. An Earth-mass planet orbiting a Centauri B. Nature 491,207–211 (2012).

41. Johnson, J. A. et al. Retired Astars and their companions. VII. 18new jovianplanets.Astrophys. J. 197 (Suppl.), 26 (2012).

42. Hatzes, A. P. et al. The Mass of CoRoT-7b. Astrophys. J. 743, 75 (2011).44. Pecaut, M. J., Mamajek, E. E. & Bubar, E. J. A revised age for upper Scorpius and the

star formation history among the F-type members of the Scorpius-Centaurus OBassociation. Astrophys. J. 746, 154 (2012).

RESEARCH LETTER

Macmillan Publishers Limited. All rights reserved©2013

Page 7: A rock composition_for_earth_sized_exoplanets

Extended Data Figure 1 | Wavelength-calibrated spectra of three stars nearthe age-sensitive Li I line (6,708 A). This line is not detected in the Kepler-78spectrum, suggesting that lithium has been depleted, consistent with an ageexceeding half a billion years for this K0 star. The lithium line is also notdetected in the 4.6-billion-year-old Sun. (Gyr, billion years; Myr, million years.)It is clearly seen in the rotationally broadened spectrum of[PZ99] J161618.0 2 233947, a star whose spectral type (G8) is similar to that ofKepler-78, but that is much younger (about 11 million years)44. Additional ironand calcium lines are labelled.

LETTER RESEARCH

Macmillan Publishers Limited. All rights reserved©2013

Page 8: A rock composition_for_earth_sized_exoplanets

Extended Data Figure 2 | Correlations between model parameters in thetransit analysis. Greyscale contours denote confidence levels, with thick blacklines highlighting the 1s, 2s and 3s contour levels. The strongest correlationsare between transit depth, scaled semi-major axis and impact parameter.

RESEARCH LETTER

Macmillan Publishers Limited. All rights reserved©2013

Page 9: A rock composition_for_earth_sized_exoplanets

Extended Data Figure 3 | Apparent radial-velocity variations of Kepler-78for the offset-slope model. The top panel shows the complete 45-day timeseries of relative radial velocities (red filled circles). Eight grey boxes highlightnights of intensive observations. The measurements from these nights areshown in the eight subpanels. In each subpanel, the radial velocities (red filledcircles) and best-fit offset-slope model (solid black line) are shown. Theradial-velocity curves for 100 randomly selected models from the MCMC chainare underplotted in grey, showing the range of variation within the modeldistribution.

LETTER RESEARCH

Macmillan Publishers Limited. All rights reserved©2013