The light climate in coastal areas is influenced by multiple factors, among them plankton biomass, and dissolved and suspended matter. Although these factors influence each other, they are still independent from each other to a certain degree, as they have different origins. Over the past decades, there have been many successful attempts to model links between phytoplankton growth and other optically active water constituents (e.g., Cahill et al., 2008;Mobley et al., 2015;Xiu & Chai, 2014). However, most attempts are challenging for long-term analysis, due to their immense complexity and computational resource constraints. There may be not enough information about all involved processes and state variables, or the model might be too cumbersome to handle over multi-year computations.Several studies indicate a decrease in water clarity over the twentieth century. These decreases have been linked to colored dissolved organic matter (CDOM)