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The Community Cloud retrieval for CLimate (CC4CL) – Part 2: The optimal estimation approach

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Table 1. The dimensions of the ORAC LUTs used in the liquid wa-ter cloud retrieval. Note that not all LUTs are functions of all vari-ables (for instance, atmospheric transmission terms are functions ofa single zenith angle only).
Figure 1. A schematic diagram of the ORAC cloud reflectance, transmission and emission operators; surface reflectance operators; and clear-sky emission profiles
Figure 2. Schematic diagrams of each of the four ORAC surface reflectance operators. Blue represents incident radiation and red representsreflected radiation
Figure 3. Fractional differences �(x), where x is either reflectance R or radiance L, between the reference forward model and the fastforward model for liquid water cloud as a function of optical thickness τ0.55,c versus effective radius re,c (µm), solar zenith angle θ0,relative azimuth angle �φ, bidirectional surface reflectance ρ0v, directional–hemispherical surface reflectance ρ0d and a combination ofhemispherical–directional and bihemispherical surface reflectance ρdv + ρdd for wavelength λ = 0.65 and effective radius re,c (µm), cloudtop pressure pc (hPa) and surface temperature Ts (K) for 3.70 and 11.00 µm.
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