Retrieving the Red Edge on Earth-like Planets with Heterogeneous Clouds and Surfaces
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http://dataverse.jpl.nasa.gov/citation?persistentId=doi:10.48577/jpl.DQRB38
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The detection and characterization of potentially habitable exoplanets is one of the chief goals of astrophysics for the coming decades. Imaging in reflected light is well suited for characterizing Earth-like planets, as much can be learned about these planets in this wavelength range (i.e., $\sim$0.3--2 $\mu$m). Several studies have been conducted to determine the abilities and limitations of reflectance spectroscopy, but most previous studies assumed a homogeneous atmospheric and surface composition. Here we investigate how heterogeneities in the atmosphere and surface of an Earth-like planet impact retrieval results. \textbf{We extend the \exorelr\ retrieval framework to include a step function for retrieving wavelength varying surface albedo. We then use it to} retrieve on visible-to-near-infrared spectra of realistic 3D Earth models with different surface features in view and varying cloud types/distributions synthesized with the Planetary Spectrum Generator. \textbf{Including the ability to fit for wavelength dependent albedo mitigates degeneracies that arise when using 1D models to analyze 3D planets, and we recover an Earth-like planet in all cases. We detect surface albedo steps at $\sim0.7$ and $\sim1.1$ $\mu$m despite clouds, both when significant lands are in view and when the spectra are averaged to account for a longer integration time. Our findings support the application of the vegetation red edge as a biosignature in the context of the Habitable Worlds Observatory.} This study highlights the importance of considering a range of---particularly wavelength-dependent---surface albedos when using reflectance spectroscopy to characterize Earth-like exoplanets.
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2026-03-29



