TY - JOUR
T1 - Impact of atmospheric nitrogen deposition on phytoplankton productivity in the South China Sea
AU - Kim, Tae Wook
AU - Lee, Kitack
AU - Duce, Robert
AU - Liss, Peter
N1 - Copyright:
Copyright 2014 Elsevier B.V., All rights reserved.
PY - 2014/5/16
Y1 - 2014/5/16
N2 - 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
AB - 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
KW - Atmospheric nitrogen deposition
KW - Chlorophyll-a
KW - Concentration weighted trajectories
KW - Ocean productivity
KW - South China Sea
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U2 - 10.1002/2014GL059665
DO - 10.1002/2014GL059665
M3 - Article
AN - SCOPUS:84901927438
VL - 41
SP - 3156
EP - 3162
JO - Geophysical Research Letters
JF - Geophysical Research Letters
SN - 0094-8276
IS - 9
ER -