Adaptation of the aerosol radiance algorithm for the atmosphere over the Baltic Sea

Details Adaptation of the aerosol radiance algorithm for the atmosphere over the Baltic Sea Adaptation of the aerosol radiance algorithm for the atmosphere over the Baltic Sea

Jan 1997

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1997spie.2956..136k&link_type=abstract

Proc. SPIE Vol. 2956, p. 136-143, Optics in Atmospheric Propagation, Adaptive Systems, and Lidar Techniques for Remote Sensing,

Physics

Optics

Scientific paper

In the standard CZCS atmospheric correction method the aerosol radiance is derived assuming that the water-leaving radiance at 670 nm is zero. This assumption, justified for water whose reflectance is determined solely by absorption (Case 1 waters), causes the errors for water whose reflectance is significantly influenced by scattering (Case 2 waters)--for example the Baltic Sea. The values of aerosol radiance are too high and the water-leaving radiance too low in comparison to the experimental ones. The relative error for the aerosol radiances (normalized to their values for 670 nm) decrease with wavelength: from 60% at 443 nm to 13% at 550 nm.

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