The radial velocity signature of tides raised in stars hosting exoplanets
Article first published online: 19 MAR 2012
DOI: 10.1111/j.1365-2966.2012.20756.x
© 2012 The Authors Monthly Notices of the Royal Astronomical Society © 2012 RAS
Issue

Monthly Notices of the Royal Astronomical Society
Volume 422, Issue 2, pages 1761–1766, May 2012
Additional Information
How to Cite
Arras, P., Burkart, J., Quataert, E. and Weinberg, N. N. (2012), The radial velocity signature of tides raised in stars hosting exoplanets. Monthly Notices of the Royal Astronomical Society, 422: 1761–1766. doi: 10.1111/j.1365-2966.2012.20756.x
Publication History
- Issue published online: 25 APR 2012
- Article first published online: 19 MAR 2012
- Accepted 2012 February 13. Received 2012 February 5; in original form 2011 July 29
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Keywords:
- hydrodynamics;
- waves;
- planet–star interactions;
- planetary systems;
- stars: solar-type
ABSTRACT
Close-in, massive exoplanets raise significant tides in their stellar hosts. We compute the radial velocity (RV) signal due to this fluid motion in the equilibrium tide approximation. The predicted RVs in the observed sample of exoplanets exceed 1 m s−1 for 17 systems, with the largest predicted signal being ∼30 m s−1 for WASP-18 b. Tidally induced RVs are thus detectable with present methods. Both the tidal fluid flow and the epicyclic motion of a slightly eccentric orbit produce an RV signal at twice the orbital frequency. If care is not taken, the tidally induced RV may, in some cases, be confused with a finite orbital eccentricity. Indeed, WASP-18 b is reported to have an eccentric orbit with small e= 0.009 and pericentre longitude
. Whereas such a close alignment of the orbit and line of sight to the observer requires fine-tuning, this phase in the RV signal is naturally explained by the tidal velocity signature of an e= 0 orbit. Additionally, the equilibrium tide estimate for the amplitude is in rough agreement with the data. Thus, the reported eccentricity for WASP-18 b is instead likely a signature of the tidally induced RV in the stellar host. Measurement of both the orbital and tidal velocities for non-transiting planets may allow planet mass and inclination to be separately determined solely from RV data. We suggest that high-precision fitting of RV data should include the tidal velocity signal in those cases where it may affect the determination of orbital parameters.

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