Controls on the distribution of fluorescent dissolved organic matter during an under-ice algal bloom in the western Arctic Ocean.

The high POC in PSW and PWW was attributable to carbon from ocean biological productivity (Figure 10 a) as indicated by a highly significant correlation between POC and Chl a ( R 2 = 0.64, n = 68; p < 0.05).

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For LPML and PSW the partitioned fluorescence components show a positive trend between ArC1 (terrestrial humic‐like) and fMW (Figure 11 d), whereas there is a positive trend between ArC3 (labile protein‐like marine FDOM) and fSIM in Figure 11 b.

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