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Analysis of the periodicity of annual extreme runoff at Datong Station, Yangtze River, China

机译:大同河,中国长江大同站年终径流周期性分析

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摘要

The periodicities of the annual maximum and minimum runoff time series at Datong hydrological station in the Yangtze River (P. R. China) were analyzed, according to the data from 1950 to 1995. The runoff of Datong hydrological station can be used to estimate the water discharges into the sea from the Yangtze River in a certain degree as there is no branch inflow from Datong station to the Yangtze Estuary. Two independent techniques were used in the analysis of time series: the conventional periodogram and the maximum entropy spectral analysis. The results reveal that the periods obtained in the time series at Datong station are related to the rainfall characteristics of the Yangtze River to a great extent. The long periods that are more than 10 years may be related to some climatic factors which are influenced by the solar activities. The short periods that are less than 10 years may be related to some factors which are affected by oceanic tides or human activities. The obtained periods not only reflect the periodicity characteristics of the water discharges into the sea from the Yangtze River, but also provide scientific evidence for the study of evolution of Datong reach of the Yangtze River.
机译:根据1950年至1995年的数据,分析了长江(PR中国)大同水文站的年度最高和最低径流时间序列的周期性。大同水文站的径流可用于估计排水在一定程度上,来自长江的大海,因为大同站到长江河口没有分支流入。在时间序列分析中使用了两种独立技术:传统时期和最大熵谱分析。结果表明,大同站时间序列中获得的时期与长江的降雨特征在很大程度上有关。超过10年的长期可能与一些受太阳能活动影响的气候因素有关。少于10年的短时间可能与受海洋潮汐或人类活动影响的一些因素有关。所获得的时期不仅反映了从长江进入大海的水中的周期性特征,而且还为长江大同达到的大同进展的研究提供科学证据。

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