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Fig. 10


H2O vertical profiles of the PACS best-fit model (see Fig. 11), in which the latitudinal distribution is a Gaussian centered around the equator with σ = 25°, and yeq = 1.1 ppb. The effect of the temperature increases in the B1 and B2 beacons is accounted for when computing the condensation level, as shown by the yellow and cyan lines (corresponding to B1 and B2, respectively). The local equatorial minimum at 1 mbar results from condensation at a temperature minimum caused by the Saturn quasi-periodic oscillation (see Fig. 4). The corresponding line area and residual maps are shown in Fig. 11.

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