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Evaluation of SHADOZ sondes, HALOE and SAGE II ozone profiles at the tropics from SAOZ UV-Vis remote measurements onboard long duration balloons

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Academic year: 2021

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Figure

Fig. 1. SAOZ long duration balloon payload. The cone at the top of the instrument defines a 360 ◦ azimuth, − 10 ◦ , +10 ◦ elevation FOV within which the full sun could be observed at sunrise and sunset without additional tracking system.
Fig. 2. Balloon trajectories and ozone profiles in 2001 (left) and 2003 (right). Blue: sunrise; Red: sunset; Green: hurricane.
Fig. 4. Percent difference between SAOZ and lidar ozone (red), and after shifting SAOZ up by 50 m (blue)
Fig. 5. Zonal variability of ozone concentration in 2001 and 2003 (Pacific only). Left: percent; Right: number density.
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