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   <subfield code="a">Climate-driven chlorophyll- a concentration interannual variability in the South China Sea</subfield>
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   <subfield code="c">[Shilin Tang, Qing Dong, Fenfen Liu]</subfield>
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   <subfield code="a">Physical forcing and biological response are highly variable over a wide range of scales in the South China Sea. The present paper analyzed interannual variability of the surface chlorophyll-a concentration of the South China Sea using NASA standard SeaWiFS monthly products from 1997 to 2007. Time series of monthly data were first smoothed using a 12-month running mean filter. An empirical orthogonal function (EOF) analysis was performed to evaluate the interannual variability. The first EOF mode is characterized by a higher surface chlorophyll-a concentration in the deep basin of the South China Sea with a maximum value southwest of Luzon Strait. The corresponding time coefficient function is highly correlated with the multivariate ENSO index (MEI). The correlation coefficient is −0.61 when the time coefficient function lags the MEI by 9months. The second EOF mode is characterized by a northwest lower chlorophyll-a concentration. The corresponding time coefficient function correlates with the MEI at a correlation coefficient equal to 0.88, with a lag of 1month. The third EOF mode shows the interannual variability of the chlorophyll-a concentration has some relationship with Indian Ocean dipole mode as well. The link between the climate and ocean biological states in the South China Sea is due to changes in upper-ocean temperature and wind field, which influence the availability of nutrients for phytoplankton growth.</subfield>
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   <subfield code="u">Key Laboratory of Digital Earth, Center for Earth Observation and Digital Earth, Chinese Academy of Sciences, 100101, Beijing, China</subfield>
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