The accurate merging of primary radiometric ocean color products such as the normalized water-leaving radiance requires combining data from various space missions, which may be affected by different uncertainties as resulting from absolute calibration and minimization of the atmospheric effects. A statisticalcorrectionschemebased on a multilinear regression algorithm is used here to remove systematic differences betweeninsituand remote-sensing measurements. The application of thecorrectionschemeto Sea-viewing Wide Field-of-View Sensor (SeaWiFS) and Moderate Resolution Imaging Spectroradiometer (MODIS) primary radiometric products improves the convergence between remote-sensing andinsitumeasurements, with the largest effects at 412 and 443 nm. Specifically, the scatter and bias of MODIS derived with respect toinsituLwnat 412 nm have shown values of 12% and 3% forcorrectedwith respect to values of 34% and -28% foruncorrecteddata, respectively. Similarly, the scatter and bias for SeaWiFS-derivedLwnat 412 nm have shown values of 14% and 4% forcorrectedwith respect to 32% and -20% foruncorrecteddata. Results at 667 nm for MODIS and at 670 nm for SeaWiFS, although displaying a reduction in the scatter of data, have shown a significant residual bias of about 11% and 17% with respect toinsituvalues. Finally, it was shown the need for restricting the application of thecorrectionschemeto data with atmospheric and marine optical features represented within the reference data set used to define the correction coefficients.
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D’Alimonte et al. (2008) studied this question.
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