Ticket #3 (new QA note)

Description

Retrievals of OMAERUV over the remote oceans in both hemispheres are affected by the wavelength dependent effect of clear water absorption. This effect yields spurious aerosol absorption and a slight over-estimation of the extinction optical depth. This artifact has been reduced by accounting for the spectral dependence of the ocean surface albedo at 354 and 388 nm. A similar effect (but smaller in magnitude) occurs over arid and semi-arid land areas. Spurious aerosol absorption retrievals may still occur when the actual surface spectral contrast differs significantly from the assumed climatological values.