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In equinox periods, most of water vapor is confined into the low\u2010middle latitudes. In aphelion periods, water vapor sublimated from the northern polar cap is confined into very low altitudes\u2014water vapor mixing ratios observed at the 0\u20135\u00a0km lower boundary of measurement decrease by an order of magnitude at the approximate altitudes of 15 and 30\u00a0km for the latitudes higher than 50\u00b0N and 30\u201350\u00b0N, respectively. The vertical confinement of water vapor at northern middle latitudes around aphelion is more pronounced in the morning terminators than evening, perhaps controlled by the diurnal cycle of cloud formation. Water vapor is also observed over the low latitude regions in the aphelion southern hemisphere (0\u201330\u00b0S) mostly below 10\u201320\u00a0km, which suggests north\u2010south transport of water still occurs. 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