Abstract
The impacts of anthropogenic nitrogen (N) deposition on the marine N cycle are only now being revealed, but the magnitudes of those impacts are largely unknown in time and space. The South China Sea (SCS) is particularly subject to high anthropogenic N deposition, because the adjacent countries are highly populated and have rapidly growing economies. Analysis of data sets for atmospheric N deposition, satellite chlorophyll-a (Chl-a), and air mass back trajectories reveals that the transport of N originating from the populated east coasts of China and Indonesia, and its deposition to the ocean, has been responsible for the enhancements of Chl-a in the SCS. We found that atmospheric N deposition contributed approximately 20% of the annual biological new production in the SCS. The airborne contribution of N to new production in the SCS is expected to grow considerably in the coming decades. Key Points N deposition contributed ~20% of the new production in the South China Sea Air masses from highly populated regions increased the Chl-a concentration © 2014. American Geophysical Union. All Rights Reserved.
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Kim, T. W., Lee, K., Duce, R., & Liss, P. (2014). Impact of atmospheric nitrogen deposition on phytoplankton productivity in the South China Sea. Geophysical Research Letters, 41(9), 3156–3162. https://doi.org/10.1002/2014GL059665
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