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Long-term MODIS observations of cyanobacterial dynamics in Lake Taihu: Responses to nutrient enrichment and meteorological factors

机译:太湖湖中蓝藻动力学的长期态度观测:对营养丰富和气象因素的反应

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We developed and validated an empirical model for estimating chlorophyll a concentrations (Chla) in Lake Taihu to generate a long-term Chla and algal bloom area time series from MODIS-Aqua observations for 2003 to 2013. Then, based on the long-term time series data, we quantified the responses of cyanobacterial dynamics to nutrient enrichment and climatic conditions. Chla showed substantial spatial and temporal variability. In addition, the annual mean cyanobacterial surface bloom area exhibited an increasing trend across the entire lake from 2003 to 2013, with the exception of 2006 and 2007. High air temperature and phosphorus levels in the spring can prompt cyanobacterial growth, and low wind speeds and low atmospheric pressure levels favor cyanobacterial surface bloom formation. The sensitivity of cyanobacterial dynamics to climatic conditions was found to vary by region. Our results indicate that temperature is the most important factor controlling Chla inter-annual variability followed by phosphorus and that air pressure is the most important factor controlling cyanobacterial surface bloom formation followed by wind speeds in Lake Taihu.
机译:我们开发并验证了估算太湖湖叶绿素(CHLA)的实证模型,以产生2003年至2013年的Modis-Aqua观测的长期CHLA和藻类绽放区时间序列。然后,基于长期时间系列数据,我们量化了蓝藻动力学对养分富集和气候条件的反应。 CHLA表现出很大的空间和时间变异性。此外,2003年至2013年整个湖泊的年平均蓝藻面积绽放区域呈现出越来越多的趋势,除2006年和2007年外,春季的高空气温度和磷水平可以提示肌菌,低风速和低风速低大气压水平有利于蓝藻表面绽放形成。发现蓝藻动力学对气候条件的敏感性因地区而异。我们的结果表明,温度是控制CHLA年间变异性的最重要因素,其次是磷,气压是控制蓝藻表面绽放形成的最重要因素,然后是太湖风速。

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