Fig. 5
Collection of 77 ratios and their errors of H37Cl over H35Cl, each obtained from 10 spectra within a single diffraction order stripe, with an error less than 400‰ measured on 29 orbits in total. The weighted mean value is δ37 Cl = −7 ± 20‰ for the Martian atmospheric HCl isotopologues is plotted with a vertical blue dashed line.
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