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

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Academic year: 2021

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Fig. 1. Radiative transfer in a case where the optical thickness is low combined with a complete cloud cover (left) and a case where the optical thickness is high with a partially covered sky (right).
Fig. 1. Radiative transfer in a case where the optical thickness is low combined with a complete cloud cover (left) and a case where the optical thickness is high with a partially covered sky (right).
Fig. 3. Left: Reflectance measured by GOME near the O 2 -A absorption band. The dotted line is a fully clouded scene, the solid line is a clear sky situation over land (the Netherlands), the dashed line is a clear sky situation over sea (the Atlantic Ocean
Fig. 3. Left: Reflectance measured by GOME near the O 2 -A absorption band. The dotted line is a fully clouded scene, the solid line is a clear sky situation over land (the Netherlands), the dashed line is a clear sky situation over sea (the Atlantic Ocean
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