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首页> 外文期刊>Remote Sensing of Environment: An Interdisciplinary Journal >Monitoring and understanding the water transparency changes of fifty large lakes on the Yangtze Plain based on long-term MODIS observations
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Monitoring and understanding the water transparency changes of fifty large lakes on the Yangtze Plain based on long-term MODIS observations

机译:基于长期MODIS观测,监测和理解长江平原五十大湖水的水透明度变化

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Various aspects of the water qualities of the large lakes in the Yangtze Plain (YP) have been studied, while the efforts have been spent on one of the most important parameters-water transparency were only limited to several large lakes. Using in situ remote sensing reflectance and Secchi-disk depth (Z(sd)) datasets, we assessed the performance of a semi-analytical model recently proposed by Lee et al. (2015) for remote sensing of the Z(sd) (Z(sd), (Lee)). The results show that a linear scaling correction over Z(sd), (Lee) (Z(sd)', (Lee)) could lead to improved agreement between remote sensing estimates and field measurements (root mean square error 35%) in the study region. The Z(sd)'(,) (Lee) scheme was then applied to MODIS/Aqua observations between 2003 and 2016 to obtain the spatial and temporal dynamics of water transparency in 50 large lakes in the YP. The long-term mean Z(sd) of the entire region was 0.39 +/- 1.17 m during the observation period, with high and low values occurring in warm and cold seasons, respectively. Of the 50 examined lakes, half demonstrated decreasing or increasing Z(sd) trends, and the number of lakes exhibiting significantly decreasing trends also comparable to the number exhibiting increasing trends. The relative contributions of the seven potential driving factors (from both human activities and natural processes) to the interannual changes in water clarity were quantified for each lake using a multiple general linear model regression analysis. The responses of Z(sd) to these drivers showed considerable differences among lakes, and human activities demonstrated significant roles in more lakes than those affected by natural variability, accounting for 50% (25/50) and 20% (10/50) of the lakes, respectively. This study provides the first comprehensive basin-scale estimate of the water transparency in the lakes in the YP, and the Z(sd) results and analysis of driving forces can provide important information for local water quality
机译:研究了长江平原(YP)中大湖泊水质的各个方面,虽然已经花费了最重要的参数 - 水透明度之一仅限于几个大湖泊。使用原位遥感反射和SECCHI-DISK DECURE(Z(SD))数据集,我们评估了Lee等人最近提出的半分析模型的性能。 (2015)用于遥感Z(SD)(Z(SD),(李))。结果表明,Z(SD),(李)(z(sd)'(z))(z(sd))可以导致遥感估计和场测量之间的协议改进(均均方误差<35%)在研究区域。然后将Z(SD)'()()()(李)方案应用于2003年至2016年间的Modis / Aqua观察,以获得yp中50个大湖泊水透明度的空间和时间动态。在观察期间,整个区域的长期平均Z(SD)为0.39 +/- 1.17 m,分别在温暖和冷季节中出现高低值。在50个被检查的湖泊中,一半证明了Z(SD)趋势的减少或增加,并且湖泊的数量表现出显着降低趋势的趋势也与表现出增加趋势的数量相当。使用多个通用线性模型回归分析,对每个湖的七个潜在驾驶因子(从人类活动和自然过程中)对水清晰度的际变化的相对贡献进行量化。 Z(SD)对这些司机的答案在湖泊中表现出相当大的差异,人类活动在更多的湖泊中表现出比受自然变异影响影响更多的湖泊,占50%(25/50)和20%(10/50)的湖泊湖泊分别。本研究提供了第一个综合盆地规模估计YP中湖泊中的水透明度,Z(SD)的结果和驱动力分析可以为局部水质提供重要信息

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