“…We assume d as the water column depth in cm (in this study, d = 500 cm), A tot (λ) = A 1 (λ) d as the total absorbance of the water column, and p°(λ) as the incident spectral photon flux density of sunlight. The sunlight p°(λ) shows a seasonal variation (see Figure 1 in the Supplementary Material, hereafter SM) (Frank and Klöpffer, 1988). CDOM is by far the main radiation absorber between 280 and 450 nm (Bracchini et al, 2010),…”