“…Because the parameters of Chl a concentration and Z SD are often used as indicators of eutrophication and turbidity in inland, coastal, and oceanic waters, many previous studies (e.g., Lewis et al, 1988;Falkowski and Wilson, 1992;Morel et al, 2007;Boyce et al, 2010Boyce et al, , 2012Doron et al, 2011) have used the empirical relationship between Z SD and Chl a concentrations to investigate phytoplankton productivity and develop algorithms for satellite ocean color remote sensing, especially in open oceans with optically simple Case I water, where phytoplankton is the primary factor affecting the IOPs of a water body (Morel and Prieur, 1977;Prieur and Sathyendranath, 1981;IOCCG, 2000). However, the variations of IOPs in optically complex coastal waters (Case II water) interacting with terrestrial waters are determined by phytoplankton, NAP, and CDOM (IOCCG, 2000;Hooker et al, 2020Hooker et al, , 2021. Although many empirical conversion factors have been reported for predicting the diffuse attenuation coefficient of the photosynthetically available radiation (PAR) (K PAR , m −1 ), which is an apparent optical property (AOP) that varies with the sun angle (Preisendorfer, 1986), there is no universal conversion factor because Z SD is affected by the bulk optical properties, especially in Case II waters (Lee et al, 2018 and references therein).…”