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Water vapour profiles from SCIAMACHY solar occultation measurements derived with an onion peeling approach

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Fig. 1. The solar occultation viewing geometry.
Figure 3a shows the derived saturation correction factor c as function of the used water vapour profile scaling factor for different tangent altitudes
Fig. 3. Results for simulated data. (a) Saturation correction factors as function of the water vapour scaling factor for different tangent altitudes
Figure 5 shows an example for retrieval results for a SCIAMACHY measurement in orbit 19 333 on 10  Novem-ber 2005
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