ACCESS: A Visual to Near-infrared Spectrum of the Hot Jupiter WASP-43b with Evidence of $\rm H_2O$, but no evidence of Na or K

TL;DR

This study presents a ground-based visual transmission spectrum of the hot Jupiter WASP-43b, revealing water vapor presence but no evidence of sodium or potassium, and suggests stellar heterogeneities influence the observed spectrum.

Contribution

First combined ground-based and space-based transmission spectrum analysis of WASP-43b, including atmospheric retrieval and stellar heterogeneity modeling.

Findings

Detection of water vapor in the atmosphere.

No significant sodium or potassium absorption detected.

Evidence of stellar heterogeneities affecting the spectrum.

Abstract

We present a new ground-based visual transmission spectrum of the hot Jupiter WASP-43b, obtained as part of the ACCESS Survey. The spectrum was derived from four transits observed between 2015 and 2018, with combined wavelength coverage between 5,300 \r{A}-9,000 \r{A} and an average photometric precision of 708 ppm in 230 \r{A} bins. We perform an atmospheric retrieval of our transmission spectrum combined with literature HST/WFC3 observations to search for the presence of clouds/hazes as well as Na, K, H$\alpha$, and $\rm H_2O$ planetary absorption and stellar spot contamination over a combined spectral range of 5,318 \r{A}-16,420 \r{A}. We do not detect a statistically significant presence of Na I or K I alkali lines, or H$\alpha$ in the atmosphere of WASP-43b. We find that the observed transmission spectrum can be best explained by a combination of heterogeneities on the photosphere of the host star and a clear planetary atmosphere with $\rm H_2O$. This model yields a log-evidence of $8.26\pm0.42$ higher than a flat (featureless) spectrum. In particular, the observations marginally favor the presence of large, low-contrast spots over the four ACCESS transit epochs with an average covering fraction $f_\text{het} = 0.27^{+0.42}_{-0.16}$ and temperature contrast $\Delta T = 132\text{ K} \pm 132\text{ K}$. Within the planet's atmosphere, we recover a log $\rm H_2O$ volume mixing ratio of $-2.78^{+1.38}_{-1.47}$, which is consistent with previous $\rm H_2O$ abundance determinations for this planet.