Mainstream swing flow rate time-order character based river type classifying method
A mainstream and time-series technology, applied in special data processing applications, water conservancy projects, instruments, etc., can solve problems affecting the effect of regulation, too general river section regulation, difficult river section division, etc., to achieve simple division method, great promotion value, The effect of enhancing the effect
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Embodiment 1
[0067] Example 1: According to formula 1, the flow range of Jianli Waterway from 1955 to 2013 is selected as Q3 / s and the flow range is Q>27000m 3 / s continuous days series data to obtain the wavelet function of Jianli Waterway, and draw the contour map of the real part of the wavelet transform coefficient of Jianli Waterway according to this function, as shown in Figure 1~2 shown.
[0068] Transform the wavelet function of Jianli Waterway according to Equation 2 to obtain the wavelet variance formula of Jianli Waterway, and draw the wavelet variance diagram of the series of continuous days of characteristic flow of Jianli Waterway, as shown in image 3 shown.
[0069] According to Equation 1, the flow range of waterways in Damazhou from 1955 to 2013 is selected as Q3 / s and the flow range is Q>27000m 3 / s continuous days series data to obtain the wavelet function of the water channel in Malaysia, and draw the contour map of the real part of the wavelet transform coefficie...
Embodiment 2
[0077] Example 2: According to formula 1, the flow range of Tianxingzhou waterway from 1955 to 2013 is selected as 25000m 3 / s3 / s and the flow range is Q>40000m 3 / s continuous days series data to obtain the wavelet function of the Tianxingzhou waterway, and draw the contour map of the real part of the wavelet transform coefficient of the Tianxingzhou waterway according to the function, as shown in Figure 9-10 shown.
[0078] Transform the wavelet function of Tianxingzhou waterway according to Equation 2 to obtain the wavelet variance formula of Tianxingzhou waterway, and draw the wavelet variance map of the series of continuous days of characteristic flow in Tianxingzhou waterway, as shown in Figure 11 shown.
[0079] According to formula 1, the discharge interval of Yangluo channel from 1955 to 2013 is selected as 25000m 3 / s3 / s and the flow range is Q>40000m 3 / s continuous days series data to obtain the wavelet function of the Yangluo waterway, and draw the contour...
Embodiment 3
[0089] Example 3: According to Formula 1, the flow range of Jiayu Waterway from 1955 to 2013 is selected as 22500m 3 / s3 / s and the flow range is Q>40000m 3 / s continuous days series data to obtain the wavelet function of Jiayu Waterway, and draw the contour map of the real part of the wavelet transform coefficient of Jiayu Waterway according to this function, as shown in Figures 17-18 shown.
[0090]Transform the wavelet function of Jiayu Waterway according to Equation 2 to obtain the wavelet variance formula of Jiayu Waterway, and draw the wavelet variance diagram of the series of continuous days of characteristic flow in Jiayu Waterway, as shown in Figure 19 shown.
[0091] According to formula 1, the flow interval of Hanjinguan Waterway from 1955 to 2013 is selected as Q>35000m 3 / s continuous days series data to obtain the wavelet function of the Hanjinguan waterway, and draw the contour map of the real part of the wavelet transform coefficient of the Hanjinguan wate...
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