Journal of Marine Sciences ›› 2012, Vol. 30 ›› Issue (4): 46-54.

Previous Articles     Next Articles

Analysis on the relations between sea surface temperature and phy toplankton Chlorophyll-a in the South China Sea

LIN Li-ru2, ZHAO Hui*1   

  1. 1. Key Laboratory of Continents-deep Sea Climate,Sources and Environments, Guangdong Ocean University, Zhanjiang 524088, China;
    2. The South China Sea Marine Engineering Survey and Environment Research Institute, SOA, Guangzhou 510300,China
  • Received:2012-03-20 Revised:2012-04-11 Online:2012-12-15 Published:2022-11-30

Abstract: Based on the Sea WiFS-derived chlorophyll-a (Chl-a) mass concentration and TRMM sea-surface temperature data from September 1997 to February 2007 from the South China Sea (SCS),seasonal variations of Chl-a and its relationship with sea surface temperature (SST) were studied. The results show that the Chl-a mass concentration of the SCS has remarkable seasonal variability. Generally the lowest phytoplankton Chl-a mass concentration(<0. 12 mg·m-3) occurs in spring or summer with low wind speed and high SST (>28 C), while the highest Chl-a mass concentration (>0. 16 mg·m-3) occurs in winter with the strongest monsoon wind and low SST (<27 C). The linear regression analysis shows that Chl-a mass concentration has obvious negative correlations with SST. Though the correlations level is different for the 4 typical sub-regions of the south,central, and west SCS and the upwelling zone southeast of V ietnam,the consistent negative correlations imply that the Chl-a mass concentration and phytoplankton biomass are controlled by vertical stratification reflected by the temperature variation. The SST is a key factor influencing the upper ocean stability and the strength of vertical exchanges, and thus controlling the variations of nutrients and phytoplankton.

Key words: South China Sea, Chlorophyll-a, sea surface temperature, seasonal variation

CLC Number: