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Comparative Analysis of Different Methods for Extracting Water Body Area of Miyun Reservoir and Driving Forces for Nearly 40 Years

机译:近40年来近40年来提取Miyun水库水体积和驱动力的不同方法的比较分析

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The Miyun Reservoir is the most important source of drinking water in Beijing, China. Based on the Landsat satellite series image, this paper compared four index methods (NDWI, RNDWI, MNDWI, AWEIsh-superimposed MNDWI) to extract the water body area of Miyun Reservoir from 1979 to 2018 to study its changes in the past 40 years. Furthermore, the internal and external driving forces of reservoir water body area change are studied by correlation analysis and catastrophe analysis. Compared to the characteristic curve of reservoir area calculation, it indicated that the AWEIsh-superimposed MNDWI method has the highest accuracy. The statistical, temporal and spatial analysis showed that the water body area changes of Miyun Reservoir are mainly divided into four distinct stages: (1) It increased in 1979-1997, which was mainly due to the increase in precipitation and the low level of economic development. In 1997, the maximum value (161.14 km(2)) was reached, which was 108.64 km(2) higher than the minimum value. (2) It shrank rapidly in 1997-2004. The areas had dropped by 101.61 km(2). By 2004, it was 59.61 km(2). The main reason is that the reservoir has suffered from persistent drought for many years after discharging water. (3) It maintained at a lower water level in 2004-2015, with an average annual area of 78 km(2). The reason is the low precipitation and rapid economic development. (4) It grew rapidly after 2015, mainly due to water from the South-to-North Water Transfer Project, coupled with the increased precipitation. By 2018, the water body area reached 125.42 km(2).
机译:Miyun水库是中国北京最重要的饮用水来源。基于Landsat卫星系列形象,本文比较了四项指数方法(NDWI,RNDWI,MNDWI,令人敬畏的MNDWI),从1979年到2018年从1979年到2018年提取Miyun水库的水体积,研究其过去40年的变化。此外,通过相关分析和灾难性分析研究了储层水体区域变化的内部和外部驱动力。与储层区域计算的特征曲线相比,表明令人敬畏的MNDWI方法具有最高的精度。统计,时间和空间分析表明,Miyun水库的水体积变化主要分为四个不同的阶段:(1)1979 - 1997年增加,主要是由于降水量和低水平的经济水平增加发展。 1997年,达到最大值(161.14公里(2)),比最小值高108.64公里(2)。 (2)1997 - 2004年迅速萎缩。该地区已跌至101.61公里(2)。到2004年,这是59.61公里(2)。主要原因是储层在排出水后多年来遭受持续干旱。 (3)它在2004 - 2015年的水平较低,年平均年面积78公里(2)。原因是低降水量和经济快速发展。 (4)2015年后迅速增长,主要是由于来自南北水转移项目的水,加上了沉淀的增加。到2018年,水体积达到125.42公里(2)。

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