Same as Fig. 5 for a meridionally uniform distribution of H2O with a mole fraction set to 4 × 10−10, after accounting for the temperature increases in the B1 and B2 stratospheric beacons caused by Saturn’s Great Storm of 2010–2011 at the time of the PACS observations. The overall fit is still poor (χ2 ∕N = 16.2) such that accounting for the temperature increases caused by Saturn’s Great Storm of 2010–2011 does not reconcile such an H2O distribution with the data.
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