Fig. 14
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Achieved χ2 values for varying carbon and oxygen mole fractions in the atmosphere versus the C/O ratio. The results are show for the Eureka! reduction of the combined NIRCam and MIRI spectrum from Hu et al. (2024), where the NIRCam flux is not allowed to vary freely and is fixed to a flux offset of +79 ppm. Each panels showcases the results for a different heat redistribution value f . The colour gradient and the numbers represent the minimal χ2.
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