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Fig. 1

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Incident stellar spectra for the different central stars. Each radiation flux is scaled to the distance where the total stellar energy input at the top of the planetary atmosphere equals the solar constant. The high-resolution spectra have been obtained from measurements in the UV and complemented at longer wavelengths with synthetic spectra. The high-resolution spectra have been binned according to the spectral resolution of the radiative transfer used in the atmospheric model (see text).

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