Long-periodic feature of runoff and its effect on riverbed in
Qiantang estuary
ZENG Jian1,2, SUN Zhi-lin1, PAN Cun-hong2, CHEN Gang2
1. College of Civil Engineering and Architecture, Zhejiang University, Hangzhou 310027, China;
2. Zhejiang Institute of Hydraulics and Estuary, Hangzhou 310020, China
In accordance with the nonstationary hydrological time series,the wavelet method was adopted to analyze the periodic feature and the trend of the runoff in the Qiantang estuary.The complex Morlet function, whose basic characteristic was discussed, was selected to transform the standardized timeseries of the annual runoff discharge.Based on the distribution of module and real of wavelet transform coefficients and wavelet variance, the prominent period of the annual runoff discharge in the Qiantang estuary is 21 years approximately, and it is predicted that the trend of the annual flow is in the low flow period from 2008 to 2010, and then the annual discharge is increase. Combined the observed topographical data, the relationships between the periodic variation of the runoff and riverbed deformation was analyzed. The results show there is a close relationship between them. The riverbed is scoured with straight alignment of river course during high flow period, and deposited with curved alignment of river course during low flow period.
CENG Jian, SUN Zhi-Lin, BO Cun-Hong, CHEN Gang. Long-periodic feature of runoff and its effect on riverbed in
Qiantang estuary. J4, 2010, 44(8): 1584-1588.
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