Constraining the oblateness of transiting planets with photometry and spectroscopy
B. Akinsanmi, S. C. C. Barros, N. C. Santos, M. Oshagh, L. M., Serrano

TL;DR
This paper explores how planetary oblateness affects spectroscopic and photometric signals during transits, finding that combined analysis enhances measurement accuracy, with spectroscopic signals detectable by high-precision instruments.
Contribution
It introduces the potential of spectroscopic Rossiter-McLaughlin signals to detect planetary oblateness and compares their effectiveness with photometric methods.
Findings
Spectroscopic signals of oblateness can reach amplitudes up to 1.1 m/s.
Photometry is generally more sensitive to oblateness detection than spectroscopy.
Combining photometry and spectroscopy yields more precise oblateness measurements.
Abstract
Rapid planetary rotation can cause the equilibrium shape of a planet to be oblate. While planetary oblateness has mostly been probed by examining the subtle ingress and egress features in photometric transit light curves, we investigate the effect of oblateness on the spectroscopic Rossiter-McLaughlin (RM) signals. We found that a giant planet, with planet-to-star radius ratio of 0.15 and Saturn-like oblateness of 0.098, can cause spectroscopic signatures with amplitudes up to 1.1 ms which is detectable by high-precision spectrographs such as ESPRESSO. We also found that the spectroscopic oblateness signals are particularly amplified for transits across rapidly rotating stars and for planets with spin-orbit misalignment thereby making them more prominent than the photometric signals at some transit orientations. We compared the detectability of oblateness in photometry and…
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