Best fit to the HIFI data for a Gaussian distribution of H2O around the equator with yeq = 2.2 × 10−7 and σ = 25°, after accounting for the effect of the temperature increases in B1 and B2 and a positive gradient for pressures higher than pgradient = 0.1 mbar and down to the condensation level with a slope n = log (y)∕log (p) = 2. The best-fit model to the PACS data from Fig. 16 is shown for comparison. Same layout as in Fig. 8 left.
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