Measured and modeled radiometric quantities in coastal waters: toward a closure

Accurate radiative transfer modeling in the coupled atmosphere-sea system is increasing in importance for the development of advanced remote-sensing applications. Aiming to quantify the uncertainties in the modeling of coastal water radiometric quantities, we performed a closure experiment to intercompare theoretical and experimental data as a function of wavelength X and water depth z. Specifically, the study focused on above-water downward irradiance E-d(lambda, 0(+)) and in-water spectral profiles of upward nadir radiance L-u(lambda, z), upward irradiance E-u(lambda, z), downward irradiance E-d(lambda, z), the E-u(lambda, z)/L-u(lambda, z) ratio (the nadir Q factor), and the E-u(lambda, z)/E-d(lambda, z) ratio (the irradiance reflectance). The theoretical data were produced with the finite-element method radiative transfer code ingesting in situ atmospheric and marine inherent optical properties. The experimental data were taken from a comprehensive coastal shallow-water data set collected in the northern Adriatic Sea. Under various measurement conditions, differences between theoretical and experimental data for the above-water E-d(lambda, 0(+)) and subsurface E-d(lambda, 0(-)) as well as for the in-water profiles of the nadir Q factor were generally less than 15%. In contrast, the in-water profiles of L-u(lambda, z), E-d(lambda, z), E-d(lambda, z) and of the irradiance reflectance exhibited larger differences [to approximately 60% for L-u(lambda, z) and E-d(lambda, z), 30% for E-d(lambda, z), and 50% for the irradiance reflectance]. These differences showed a high sensitivity to experimental uncertainties in a few input quantities used for the simulations: the seawater absorption coefficient; the hydrosol phase function backscattering probability; and, mainly for clear water, the bottom reflectance. (C) 2003 Optical Society of America.