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Fig. 27

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Comparison with laboratory data. CO2 band in Ganymede spectra at the pole (60–75°N; dotted light gray lines) and the equator (0–15°N; dot-dashed gray lines) of the leading hemisphere compared with transmission spectra from Berlanga et al. (2016; carboneous chondrites), Bekhti et al. (2021; zeolites), Ehrenfreund et al. (1999; CO2 ice and CO2-H2O ice mixture) and Fleyfel & Devlin (1991; CO2 clathrates). Some spectra are vertically shifted for the sake of clarity.

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