Upgrade to Pro — share decks privately, control downloads, hide ads and more …

The Stellar Variability Noise Floor – ISSI 2021

Brett Morris
September 21, 2021

The Stellar Variability Noise Floor – ISSI 2021

ISSI Workshop on “Getting Ultra-Precise Planetary Radii with PLATO: The Impact of Limb Darkening and Stellar Activity on Transit Light Curves,” Bern, Switzerland, September 2021

Brett Morris

September 21, 2021
Tweet

More Decks by Brett Morris

Other Decks in Science

Transcript

  1. The Stellar Variability Noise Floor Brett Morris (⭐/🌎) with Monica

    Bobra (☀), Eric Agol (🌎), Yu Jin Lee (🎓) and Suzanne Hawley (⭐) Sept 21, 2021 1
  2. Ongoing and Recent Projects • Olin Wilson Legacy Survey: Decade-scale

    CaII H & K monitoring of planet-hosting stars • Starspot coverage of FGKM stars ◦ High resolution spectroscopy [Direct: 1; CCF: 2], ◦ Rotational modulation via photometry [ABC: 3] • Joint inference of phase curve parameters in presence of (possible?) stellar activity ◦ 55 Cnc e with CHEOPS [4] ◦ Kepler-7 b with Kepler [5] • Planet hunts for objects orbiting white dwarfs [6] 2
  3. Case Study: 55 Cnc • Slowly rotating K dwarf host

    star to five planets (39 d) • Planet e is a transiting super-Earth with a density consistent with rock (6.6 g/cm3) • Phase curve of planet cannot be explained strictly by reflection from the planet’s surface • Is stellar magnetic activity to blame? Morris+ (2021) Raw Detrend
  4. Case Study: 55 Cnc Activity maximum Activity minimum OWLS Keck/HIRES

    (In prep) OWLS observations confirm CHEOPS observations occurred near activity maximum Activity maximum
  5. Planetary radius Three forms of variability during transits may affect

    transit radius measurements 1. Variability caused by non-uniformity in the surface brightness of the star which is being occulted by the planet 2. Variability due to temporal variations in the total flux emitted by the unocculted star. 3. Limb-darkening affects the depth of the transit depending on impact parameter These three effects limit how well we can measure the planet-star radius ratio. 8
  6. SDO/HMI • Observes six wavelengths centered on Fe I spectral

    line at 6173 Å • All observations available at http://jsoc.stanford.edu • Focus on: ◦ Observations near active minimum (2018) ◦ b=0 -> maximal granule contrast, minimal spot contamination 9
  7. Primary objectives 1. Effects of granulation and super-granulation on transit

    photometry of Earth a. Simulated “without” photon noise or time variations 2. Effects of solar oscillations, granulation, and activity (all together!) a. Observed directly with photon noise 10
  8. Granules: 0.5 Mm Supergranules: 16 Mm Granulation processes are stochastic

    but have typical length and turnover timescales which stay roughly constant -> model them with a Gaussian process Types of granulation Granule: 0.5 Mm Super- Granule: 16 Mm Earth: 6 Mm 12
  9. Static sun, moving Earth • Simulate transits across 282 deconvolved

    images of the inactive Sun • Fit each transit with a Mandel & Agol transit model • Residuals typically have standard deviations of 0.5 ppm, and a typical range is 2 - 4 ppm 13
  10. Static sun, moving Earth • Typical uncertainty on the exoplanet

    radius is 0.02% R p . We consider this a noise floor, or a lower limit, since we modelled the granulation pattern from a synthetic transit across a single, static image. • Autocorrelation timescale in residuals: 18 minutes ◦ Given orbital velocity, 18 minute transit time corresponds to 16 Mm occulted region -> consistent with supergranule size ◦ Supergranulation turnover timescale is 2 days, so supergranules are ~constant during an Earth transit 15
  11. Static sun, moving Earth Expectations for other spectral types: •

    Granule size -> (Surface gravity)-1 ◦ Smaller star = smaller granules = smaller residual signal • Supergranulation: ? ◦ Amplitude is small, horizontal scales are large -> hard to simulate 16
  12. • Take four days of 45 second SDO/HMI continuum intensity

    images • Disk-integrate to compute photometry • Inject an earth transit (full duration ~ 13 hrs; ingress/egress duration ~ 15 min) Dynamic sun, moving Earth 17
  13. • Oscillations+granulation+activity are similar in scale to the transit depth

    • Radius uncertainty is about 3.6% Dynamic sun, moving Earth 18
  14. Three-way degeneracy Impact parameter, planet radius, limb-darkening Ingress/egress duration becomes

    too long and can be excluded by the observations Long tail for larger impact parameter solutions 21
  15. Mitigation strategies for PLATO • Careful propagation of the stellar

    density measured via asteroseismology into the measurement of the exoplanet's orbital parameters • Auxiliary IR observations of PLATO targets where stellar variability and limb-darkening are weaker to measure precision exoplanet radii and orbital parameters • A longer extended mission to improve upon the radius measurement uncertainties 22
  16. Conclusions • Transit residuals show p-mode oscillations and granulation, of

    order 100 ppm in amplitude. • We find that the brightness variations due to (super/)granulation only is of order 2-4 ppm, to the in-transit photometry • Radius uncertainties of 3.6% are possible with photon noise-limited photometry with a Gaussian process 23