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Research on long-term streamflow variation characteristics in Poyang Lake watershed based on wavelet analysis

机译:基于小波分析的Po阳湖流域长期流量变化特征研究

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Based on the monthly runoff series (1955–2003) of the three gauging stations in Poyang Lake watershed, the wavelet transform method was adopted to analyze the temporal trend and periodic variation of the streamflows in the watershed. Result from Multi-Resolution Analysis (MRA) using the Db3 wavelet function indicates that the long-term trend of streamflow in the Poyang Lake watershed show ascends before 1998 while descends thereafter, and the descending rate is slower than that of rising rate. Causes for this mainly come from the long-term uptrend of precipitation and downtrend of actual evapotranspiration, and both trends turn over at 1998. Periodicity analysis from continuous wavelet transform (CWT) revealed that there exist 25–26 years' first dominant periods and 8 years, 3–4 years' sub-dominant periods at all three stations. According to the variation of periodicity, it can be anticipated that the Poyang Lake watershed will be in the relative arid climate in the next 10 years, and the higher frequency and severity of droughts will persist. The watershed will enter into a humid climate and high-flow period at about 2018.
机译:基于Po阳湖流域三个测站的月径流序列(1955-2003),采用小波变换方法分析了流域的径流的时间趋势和周期性变化。利用Db3小波函数进行的多分辨率分析(MRA)结果表明,1998阳湖流域的长期水流趋势在1998年前呈上升趋势,其后呈下降趋势,其下降速度比上升速度慢。造成这种现象的原因主要是降水的长期上升趋势和实际蒸散量的下降趋势,并且两种趋势都在1998年发生了转变。连续小波变换(CWT)的周期性分析显示,存在25-26年的第一优势期和8三个站的3年至3年的主要时间。根据周期性变化,可以预见,未来10年years阳湖流域将处于相对干旱的气候中,干旱的频率和严重性将持续存在。该分水岭将在2018年左右进入潮湿气候和高流量时期。

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