Fig. 5

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Comparisons of the normalised HCl and H2O VMR abundances observed by the NOMAD spectrometer in MY34–35 (Aoki et al. 2021) and the 77 1D photochemistry model runs with the standard climatolog-ical and MY34 datasets of the MCDv6.1, and MY34 with approximately colocated ACS TIRVIM aerosols and NOMAD/ACS NIR H2O profiles. Gradients (m) and correlation coefficients (R) for the lines of best fit are as follows. For all model runs, m = 0.82 and R = 0.854. For NOMAD MY34, m = 0.91 and R = 0.92. For NOMAD MY35, m = 0.80 and R = 0.90. This analysis follows Aoki et al. (2021).
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