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SPATIAL AND TEMPORAL VARIABILITY OF CHLOROPHYLL A DURING THE AUSTRAL SUMMER IN PRYDZ BAY, ANTARCTICA
Jin Siyun, Pan Jianming, Han Zhengbing
2012, 24 (4):
361-371.
DOI: 10.3724/SP.J.1084.2012.00361
Making use of the chlorophyll-a (Chl-a) and sea surface temperature (SST) derived from SeaWiFs and MODIS satellite ocean color date, and combining with the data in situ by Chinare, it discussed the distributions of SST, Chl-a and nutrients in austral summer in Prydz Bay, and the influencing factors were analyzed. As it turns out, the distribution of surface Chl-a in Prydz Bay showed significant characteristics, the surface Chl-a concentrations decreased offshore. In the shelf area, the bloom of phytoplankton was affected by the ablation of sea ice and the supply of nutrients. In the slope area, the growth of phytoplankton was mainly affected by the hydrological conditions. And in outside the Bay, the Chl-a concentration was much lower, and it was influenced by the lack of iron probably. In the last decade, the average of Chl-a concentrations of remote sensing were 1.40, 0.44 and 0.25 mg/m3 from the shelf to the outside, respectively. In astral summer, a high positive correlation between Chl-a with SST was founded in Prydz Bay, R2=0.505. The annual concentration variation showed that the Chl-a trended strongly related with SST, revealing that the temperature was the main factor. Using the relationship between the Multivariate ENSO Index (MEI) and the Chl-a concentration inner shelf area, it demonstrated that Chl-a concentration was much higher when EL Nino happened than that when La Nina happened, revealing that the growth and reproduction of phytoplankton at high-latitude has remarkable response with the ENSO occurred at Middle and low latitudes.
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