首页> 外文期刊>Geomatics,Natural Hazards & Risk >The use of HJ-1A/B satellite data to detect changes in the size of wetlands in response in to a sudden turn from drought to flood in the middle and lower reaches of the Yangtze River system in China
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The use of HJ-1A/B satellite data to detect changes in the size of wetlands in response in to a sudden turn from drought to flood in the middle and lower reaches of the Yangtze River system in China

机译:利用HJ-1A / B卫星数据检测中国长江流域中下游因干旱突然转变为洪水而引起的湿地面积变化

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This study analysed the response in the size of wetlands to a sudden turn from drought to flood along the Yangtze River system in China. The wetlands and their spatial distributions in the provinces of Hubei, Hunan, Jiangxi, Anhui and Jiangsu for three periods (April and May 2010, April and May 2011 and June and July 2011) were identified by the artificial visual interpretation of charge-coupled device images obtained in 2010 and 2011 by the HJ-1A and HJ-1B satellites. The sizes of the wetland areas of all five provinces in the three periods were 30,087.10, 23,427.68 and 31,346.49????km 2 , respectively, with the largest changes occurring in Jiangxi. Changes in the mean standardized precipitation index (SPI) and its patterns of spatial distribution had similar trends to the changes in the size of the wetlands of each province in the three periods. SPI was positively correlated ( R 2 = 0.360, p < 0.05) with changes in the proportions of the wetlands during the drought. The mean SPI of the final period after the flood was positively correlated ( R 2 = 0.406, p < 0.01) with changes in the proportions of wetlands. Poyang Lake and Dongting Lake were impacted most by the flood, and Hongze Lake and Caohu Lake were the least affected.
机译:本研究分析了中国长江沿岸湿地面积对干旱突然转变为洪水的响应。通过电荷耦合装置的人工视觉判别,确定了湖北,湖南,江西,安徽和江苏三个省(2010年4月和2010年4月,2011年4月和2011年5月以及2011年7月)的湿地及其空间分布。 HJ-1A和HJ-1B卫星在2010年和2011年获得的图像。这三个时期所有五个省的湿地面积分别为30,087.10、23,427.68和31,346.49?km 2,变化最大的是江西。在这三个时期,平均标准化降水指数(SPI)及其空间分布格局的变化与各省湿地面积的变化具有相似的趋势。 SPI与干旱期间湿地比例的变化呈正相关(R 2 = 0.360,p <0.05)。洪水后最后一个时期的平均SPI与湿地比例的变化呈正相关(R 2 = 0.406,p <0.01)。阳湖和洞庭湖受洪水影响最大,洪泽湖和草湖受到的影响最小。

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