Measuring the Mass of an Earth-size Planet Using a Gaussian Process Model of Precise Radial Velocities
Application of a new nonparametric model to combine two independent datasets, remove a stellar activity signal, and uncover the much weaker planet signal hiding underneath.
• previously used in exoplanet studies (Gibson et al. 2012, Petigura et al. 2013, concurrently with Haywood et al. 2014) • Depends only on choice of covariance kernel Gibson et al. (2012)
= 1.92 ± 0.25 m s 1 Adopted Quasiperiodic Model Parameters HYPERPARAMETER HIRES HARPS-N h: amplitude -8.2 +27/-11 m/s 4.4 +2.9/-10.5 m/s θ*: period 12.78 ± 0.03 days 12.78 ± 0.04 days w: roughness 0.32 +0.11/-0.07 0.30 +0.10/-0.07 λ*: lengthscale 1.8e23 +3.6e30/-1.8e23 days 23 +22/-17 days σ: stellar jitter 2.1 ± 0.3 m/s -0.02 ± 1.3 m/s
al. (2013) • • Iron fraction 0.32 ± 0.26, suggesting formation possibly similar to Earth’s • Results broadly consistent with Hatzes (2014), who analyzed both datasets with variant on Floating Chunk Offset model ⇢pl = 6.1+1.9 1.4 g cm 3 Black cross: previous estimate Red point: This work Gray points: Other small known exoplanets Green points: Earth/Venus/Mars Mpl = 1.83 ± 0.27M M HIRES = 1.69 ± 0.41M M HARPS N = 1.86+0.38 0.25 M Mpl = 1.83 ± 0.27M
to better extract planetary Doppler amplitude • Found separate quasiperiodic kernel with stellar jitter terms describe datasets best • Converted Doppler amplitude into 2.5-σ improvement in mass calculation over Howard et al. (2013) • Iron mass fraction of 0.32 ± 0.26 suggests Kepler-78b is most likely Earthlike in composition. • True benefit of this technique: nonparametric model of stellar activity.