The present paper dealt with the annual dynamics of the absorption coefficient of
chromophoric dissolved organic matter at 440 nm {aCDOM(440)} during February 2015 to January
2016 in the continental shelf of northern Bay of Bengal (nBoB) for the
first time. Sea surface
salinity (SSS), chlorophyll-a (Chl-a), total suspended matter (TSM) were also analyzed. It was
hypothesized that CDOM should exhibit significant spatial and temporal variability in this region.
aCDOM(440) and spectral slope ranged between 0.1002 m1—0.6631 m1 and 0.0071 nm1—
0.0229 nm1 respectively during the entire study period. Higher values of aCDOM(440) were
observed in the near shore stations and gradually decreased towards the offshore. Significant
seasonal variability of aCDOM(440) was observed between the monsoon and non-monsoon seasons
( p < 0.05). Thus the framed hypothesis was successfully accepted by means of the present study.
The CDOM was mainly found to be of allochthonous character in this region. aCDOM(440) portrayed
a significant negative linear relationship with SSS (R2 = 0.80; p < 0.05) implying conservative
mixing of marine and terrestrial end members. However, examining the spatial variability of the
relationship, it was observed that this relationship was significant only in the nearshore stations. While examining the seasonal variability of this relationship, it was found to be most significant
during the monsoon (R2 = 0.81; p < 0.05). Thus it was inferred that whenever the SSS gradient was
higher, the relationship between aCDOM(440) and SSS was found to be most significant.
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