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Retrieval methods of effective cloud cover from the GOME instrument: an intercomparison

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Academic year: 2017

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Table 1. Spectral range of the Polarisation Measurement Detector (PMD) channels.
Fig. 2. Image showing the reflectance in 16 PMD sub-pixels inside each of a number of GOME pixels over the Netherlands (1 August 1997, pixel nrs: 480–510 (north to south), tracknr 104).
Table 2. The OCRA IMAU offset factors O(λ) and scaling factors S(λ) per PMD channel used in this study.
Fig. 4. An RGB image of the minimum reflectance surface databases of an area between 0S - 25S and 145W - 80W (Pacific Ocean) for OCRA (top) and PCRA (bottom).
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