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<sup>15</sup>N enrichment in the surface Particulate Organic Nitrogen of the north-eastern Arabian Sea from the middle to the waning phase of the winter monsoon: possible causes

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Academic year: 2017

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Table 1. Particulate organic nitrogen (PON) and nitrogen isotopic composition (δ 15 N) observed during present study.
Fig. 1. Stations sampled during (a) January and (b) late February–early March.
Fig. 2. Hydrodynamic conditions during sampling (a) sea surface temperature-January (b) sea surface temperature-late February–early March (c) temperature based mixed layer depth–
Fig. 3. Relationship between (a) PON and δ 15 N (b) δ 15 N and nitrate during present study.
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