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Estimating cloud optical thickness and associated surface UV irradiance from SEVIRI by implementing a semi-analytical cloud retrieval algorithm

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Table 1. Error statistics between estimated SCOT from SEVIRI and SCOT from CloudSat.
Table 2. Error statistics between estimated surface level UV irradiance and measurements.
Fig. 1. Background surface albedo (A in %) for June 2006 from minimum value compositing method
Fig. 2. The parameterised transmittance given by Eq. (6) (continuous curve) and the transmit- transmit-tance computed from TUV model simulations (symbols).
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