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monsoon winds. A high coastal Chl-
a
band is sustained due to coastal
upwelling derived from Ekman offshore transport of strong winds with lower
temperature, while the high Chl-
a
in the western SCS basin is related to
upwelling induced by wind stress.
Acknowledgements
The present research was supported by: a, “Major Project of Knowledge
Innovation (No. KZCX3-SW-227-3)” funded by the Chinese Academy of
Sciences (CAS); b, the National Natural Science Foundation of China
(NSFC40576053); c, “One Hundred Talents Program” (Ybjh0403) of
CAS; and d, “International Cooperation Program (Knowledge Innovation
Group)” of CAS awarded to Professor DanLing TANG.
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