Budget of riverine nitrogen over the East China Sea shelf

Riverine nitrogen loading to the continental shelf sea is important for terrestrial-marine linkage and global nitrogen cycling and leads to serious marine environmental problems. The budget and cycle of riverine nitrogen over the continental shelf in the East China Sea (ECS) are unknown. Using the tracking technique within a physical-biological coupled model, we quantified the nitrogen budgets of riverine dissolved inorganic nitrogen (DIN) and particulate organic nitrogen (PON) over seasonal to annual scales in the ECS, especially from the Changjiang River, which plays a dominant role in riverine nitrogen input. The horizontal distributions of the Changjiang DIN and PON generally followed the Changjiang diluted water and coastal currents and were affected by stratification in the vertical direction. Their inventory variations were dominated by biological fluxes and modulated by physical ones, and changed most dramatically in the inner shelf among three subregions. Less than half of DIN were converted to PON with most of the rest leaving the ECS through lateral transport pathways, among which the flux through the Tsushima Strait was dominant. With the increasing loading of the Changjiang DIN flux from the 1980s-2010s, lateral transports rather than PON production increased due to limited primary production. Approximately 60 % of the produced PON exported to the sediment and 34 % went to the Tsushima Strait. According to the export production, the DIN from the Changjiang River contributed 12-42 % to the ECS carbon sequestration.

Automated summary

Using a physical-biological coupled model, researchers quantified the nitrogen budgets of riverine dissolved inorganic nitrogen (DIN) and particulate organic nitrogen (PON) in the East China Sea (ECS). The Changjiang River plays a dominant role in nitrogen input, with the horizontal distributions of Changjiang DIN and PON being influenced by coastal currents and vertical stratification. Overall, less than half of DIN is converted to PON, with most leaving the ECS through lateral transport pathways, especially through the Tsushima Strait.