2018
DOI: 10.1016/j.jag.2018.01.020
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Evaluating the impact of sea surface temperature (SST) on spatial distribution of chlorophyll-a concentration in the East China Sea

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Cited by 51 publications
(25 citation statements)
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References 31 publications
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“…Within a certain temperature range, the positive correlation between Chl-a concentration and SST is significant, i.e., decreasing SST will inhibit the growth of phytoplankton, and Chl-a concentration will also decrease; on the contrary, as SST increases, phytoplankton grows vigorously, and the concentration of Chl-a also increases. However, excessively high temperatures will inhibit the rise of the Chl-a concentration, which is the reason why the concentration of Chl-a on 20 July is lower than that on December 17; this finding is consistent with previous research results [69][70][71][72][73]. The change of SSS is almost the opposite of that of the Chl-a concentration.…”
Section: Temporal Variationsupporting
confidence: 91%
“…Within a certain temperature range, the positive correlation between Chl-a concentration and SST is significant, i.e., decreasing SST will inhibit the growth of phytoplankton, and Chl-a concentration will also decrease; on the contrary, as SST increases, phytoplankton grows vigorously, and the concentration of Chl-a also increases. However, excessively high temperatures will inhibit the rise of the Chl-a concentration, which is the reason why the concentration of Chl-a on 20 July is lower than that on December 17; this finding is consistent with previous research results [69][70][71][72][73]. The change of SSS is almost the opposite of that of the Chl-a concentration.…”
Section: Temporal Variationsupporting
confidence: 91%
“…The positive correlation between SST and Chl-a may be explained by the fact that increased SST enhances the water stratification, which in turn increases the light availability in turbid coastal waters, and thus promotes the growth of phytoplankton [19]. Similar results were obtained by Ji et al [35] for the coastal waters of East China Sea (north coast of Jiangsu Province, Yangtze River estuary region, and the Hangzhou Bay) using the DINEOF reconstructed monthly MODIS/Aqua Chl-a and SST datasets during 2003-2016. In the Bay of Bengal, where phytoplankton productivity is highly influenced by river discharge, Jutla et al [36] reported positive correlations between monthly SeaWiFS Chl-a and SST from 1997 to 2009.…”
Section: Eof Analysis: Monthly Variability Of Chl-asupporting
confidence: 59%
“…On the other hand, some others have reported that vegetation indices constructed in the near-infrared band were highly correlated with total chlorophyll content [64,65]. Although the vegetation indices constructed in the near-infrared band were highly accurate for the inversion of chlorophyll content [66,67] in the salt treatment in our study, this needs to be further refined in the future study. In the present study, vegetation indices D_RVI and D_NDVI were more suitable for than the red edge parameters of Suaeda salsa for estimating the total chlorophyll content under different salt conditions (Figure 7).…”
Section: Mechanisms and Potential For Monitoring Plant Stress Using Rcontrasting
confidence: 56%