Fig. 14
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Uranus: Vertical cross sections of temperature at spring equinox (Ls=0°) (a) and northern summer solstice (Ls=90°) (b). The temperature observed at autumn equinox and winter solstice is almost similar (because of its slightly non circular orbit) as spring equinox and summer solstice but the maximum and minimum temperature is reversed in latitude (Fig. 15).
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