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Transmission spectroscopy measures wavelength-dependent photon attenuation during planetary transit. Each spectral channel probes a distinct effective optical path length through the atmosphere.
Low gravity results in a large atmospheric scale height, enhancing photonic detectability.
Data correspond to binned transmission spectra from public JWST ERS releases, shown with 1σ uncertainties.
Distinct absorption bands correspond to molecular opacities and Rayleigh scattering at short wavelengths.
Isothermal hydrostatic atmosphere:
H = kBT / (μg)
This model isolates photonic sensitivity without full retrieval degeneracies.
Independent instruments show consistent photonic signatures, validating instrumental calibration.