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
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
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
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
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
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
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
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
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
Granule size -> (Surface gravity)-1 ◦ Smaller star = smaller granules = smaller residual signal • Supergranulation: ? ◦ Amplitude is small, horizontal scales are large -> hard to simulate 16
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
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