J/A+A/621/A49            K2-18 HARPS time-series               (Cloutier+, 2019)

Confirmation of the radial velocity super-Earth K2-18c with HARPS and CARMENES. Cloutier R., Astudillo-Defru N., Doyon R., Bonfils X., Almenara J.M., Bouchy F., Delfosse X., Forveille T., Lovis C., Mayor M., Menou K., Murgas F., Pepe F., Santos N.C., Udry S., Wuensche A. <Astron. Astrophys. 621, A49 (2019)> =2019A&A...621A..49C 2019A&A...621A..49C (SIMBAD/NED BibCode)
ADC_Keywords: Stars, double and multiple ; Exoplanets ; Radial velocities Keywords: techniques: radial velocities - planets and satellites: fundamental parameters - planets and satellites: detection - methods: data analysis - planets and satellites: individual: K2-18 Abstract: In an earlier campaign to characterize the mass of the transiting temperate super-Earth K2-18b with HARPS, a second, non-transiting planet was posited to exist in the system at ∼9-days. Further radial velocity follow-up with the CARMENES spectrograph visible channel revealed a much weaker signal at 9-days, which also appeared to vary chromatically and temporally, leading to the conclusion that the origin of the 9-day signal was more likely related to stellar activity than to a planetary presence. Here we conduct a detailed re-analysis of all available RV time-series -- including a set of 31 previously unpublished HARPS measurements -- to investigate the effects of time-sampling and of simultaneous modelling of planetary plus activity signals on the existence and origin of the curious 9-day signal. We conclude that the 9-day signal is real and was initially seen to be suppressed in the CARMENES data due to a small number of anomalous measurements, although the exact cause of these anomalies remains unknown. Investigation of the signal's evolution in time with wavelength and detailed model comparison reveals that the 9-day signal is most likely planetary in nature. Using this analysis we reconcile the conflicting HARPS and CARMENES results and measure precise and self-consistent planet masses of mp,b=8.63±1.35 and mp,csin(ic)=5.62±0.84 Earth masses. This work, along with the previously published RV papers on the K2-18 planetary system, highlights the importance of understanding the time-sampling and of modelling the simultaneous planet plus stochastic activity, particularly when searching for sub-Neptune-sized planets with radial velocities. Description: HARPS spectroscopic time-series of K2-18 including radial velocities and spectroscopic activity indices. Objects: -------------------------------------------------- RA (2000) DE Designation(s) -------------------------------------------------- 11 30 14.52 +07 35 18.3 K2-18 = EPIC 201912552 -------------------------------------------------- File Summary: -------------------------------------------------------------------------------- FileName Lrecl Records Explanations -------------------------------------------------------------------------------- ReadMe 80 . This file tablea1.dat 95 106 K2-18 HARPS time-series -------------------------------------------------------------------------------- See also: J/A+A/608/A35 : K2-18 HARPS time-series (Cloutier+, 2017) Byte-by-byte Description of file: tablea1.dat -------------------------------------------------------------------------------- Bytes Format Units Label Explanations -------------------------------------------------------------------------------- 1- 11 F11.6 d Time Timestamp (BJD-2450000) 13- 18 F6.2 m/s RV Radial velocity 20- 23 F4.2 m/s e_RV Radial velocity uncertainty 25- 30 F6.2 m/s blueRV Radial velocity from blue orders 32- 36 F5.2 m/s e_blueRV Radial velocity from blue orders uncertainty 38- 43 F6.2 m/s redRV Radial velocity from red orders 45- 49 F5.2 m/s e_redRV Radial velocity from red orders uncertainty 51- 57 F7.5 --- NaD Sodium doublet activity index 59- 65 F7.5 --- e_sigNaD Sodium doublet activity index uncertainty 67- 73 F7.5 --- Halpha H-alpha activity index 75- 81 F7.5 --- e_Halpha H-alpha activity index uncertainty 83- 87 F5.3 --- FWHM Full width at half maximum of the cross-correlation function 89- 95 F7.3 --- BIS Bi-sector inverse slope of the cross-correlation function -------------------------------------------------------------------------------- Acknowledgements: Ryan Cloutier, cloutier(at)astro.utoronto.ca
(End) Ryan Cloutier [UofT, Canada], Patricia Vannier [CDS] 02-Nov-2018
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