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Monitoring the lowermost tropospheric ozone with thermal infrared observations from a geostationary platform: performance analyses for a future dedicated instrument

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Figure

Table 7. Same as Fig. 6 but for the surface −3 km TOCs.MilanParisBerlinAmsterdam
Fig. 3.Fig. 3. Mean integral averaging kernel functions for the surface–3 km (blue), 4–6 km (red) and surface–6 km (green) TOCs, for allpixels in the data set having a thermal contrast between 0 and 1.0 K
Table 2. Mean DOFs for surface–6 km and surface–3 km for land/day, land/night, sea/day and sea/night pixels, calculated over the wholedata set, on a 1 h revisit time basis.
Fig. 4. Average surface–6 km TOC for 5–28 August 2009. From left to right: raw and AK-smoothed MOCAGE pseudo-reality, MAGEAQ-TIR pseudo-observations, differences of MAGEAQ-TIR pseudo-observations with respect to raw MOCAGE pseudo-reality
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