The effects of oceanic whitecaps on ocean-color imagery are simulated
and inserted into the proposed Sea-Viewing Wide-Field-of-View Sensor (
SeaWiFS) atmospheric-correction algorithm to understand its tolerance
to error in the estimated whitecap contribution. The results suggest t
hat for wind speeds less than or equal to 10-12 m/s, present models th
at relate whitecap reflectance to wind speed are sufficiently accurate
to meet the SeaWiFS accuracy goal for retrieval of the water-leaving
radiance in the blue, when the aerosol scattering is weakly dependent
on wavelength. In contrast, when the aerosol scattering has a strong s
pectral signature, the retrievals will meet the goal only when the whi
tecap reflectance is underestimated.