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Improvement of retrieved reflectance in the presence of clouds

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Figure

Figure 2.1: Atmospheric transmission spectra showing windows available for earth observations.[Schott, 1997]
Figure 3.32: Process to apply adaptive ELM to real imagery.
Figure 3.34: Modeled vs. measured total SKY radiance. Modeled radiance created using clear skyconditions, shown in black.
Figure 3.35: The PARABOLO III instrument can be used to obtain directional downwelling terms,and was developed by the Jet Propulsion Laboratory [Bruegge et al., 2000].
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