Granulation on a quiet K dwarf: HD 166620 I. Spectral signatures as a function of line-formation temperature
Ancy Anna John, Khaled Al Moulla, Niamh K. O'Sullivan, Jay Fitzpatrick, Andrew Collier Cameron, Ben S. Lakeland, Michael Cretignier, Annelies Mortier, Tim Naylor, Joe Llama, Suzanne Aigrain, Christian Hartogh, Shweta Dalal, Heather M. Cegla, Christopher A. Watson, Xavier Dumusque, Aldo F. Martinez Fiorenzano
TL;DR
This study targets granulation as a limiting RV noise source in extreme-precision RV measurements by observing the magnetically quiet K-dwarf HD 166620 with HARPS-N (and contemporaneously EXPRES). After identifying and removing a new instrumental signature linked to CCD illumination and fibre injection, the authors detect granulation using structure-function analysis and a one-component Gaussian Process with an aperiodic SHO kernel, obtaining a characteristic timescale of $43.5 \,\pm\, 16.9$ minutes and a granulation amplitude of $0.23 \,\pm\, 0.07$ m s$^{-1}$. By constructing temperature-sensitive RVs with two formation-depth bins using both ${ m CCF}_{T}$ and ${ m LBL}_{T}$ methods, they show granulation signals are present in both depth regimes, but the cooler bin (shallower layers) aligns more closely with predictions. The results highlight depth-dependent granulation signatures in a K-dwarf, offer a practical path to depth-resolved granulation diagnostics for EPRV, and emphasize the importance of correcting instrumental systematics in precision RV work.
Abstract
As Radial velocity (RV) spectrographs reach unprecedented precision and stability below 1 m/s, the challenge of granulation in the context of exoplanet detection has intensified. Despite promising advancements in post-processing tools, granulation remains a significant concern for the EPRV community. We present a pilot study to detect and characterise granulation using the High-Accuracy Radial-velocity Planet Searcher for the Northern hemisphere (HARPS-N) spectrograph. We observed HD166620, a K2 star in the Maunder Minimum phase, intensely for two successive nights, expecting granulation to be the dominant nightly noise source in the absence of strong magnetic activity. Following the correction for a newly identified instrumental signature arising from illumination variations across the CCD, we detected the granulation signal using structure functions and a one-component Gaussian Process (GP) model. The granulation signal exhibits a characteristic timescale of 43.65$\pm$15.8 minutes, within one $σ$, and a standard deviation of 22.9$\pm$0.77 cm/s, with in three $σ$ of the predicted value. By examining spectra and RVs as a function of line formation temperature , we investigated the sensitivity of granulation-induced RV variations across different photospheric layers. We extracted RVs from various photospheric depths using both the line-by-line (LBL) and cross-correlation function (CCF) methods to mitigate any extraction method biases. Our findings indicate that granulation variability is detectable in both temperature bins, with the cooler bins, corresponding to the shallower layers of the photosphere, aligning more closely with predicted values.
