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A 12-year long global record of optical depth of absorbing aerosols above the clouds derived from the OMI/OMACA algorithm

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Figure

Figure 1. Simulation of UVAI (y axis) vs. reflectance at 388 nm (x axis) for the different pairs of ACAOD and COD (both at 388 nm) forthe carbonaceous (a) and spheroidal shape dust aerosols (b)
Figure 2. (a) Geographical boundaries of the 14 regions considered for calculating corresponding regional values of SSA (388 nm)
Figure 3. A general flowchart of the OMACA algorithm.
Table 1. A description of the OMACA algorithm retrieval quality flags.
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