根据利津站1950-2003年长系列的水、沙实测资料,运用统计分析方法对比分析研究了长系列及近期(1986-2003年)黄河入海口区水、沙通量的季节性变化、年际变化以及水、沙通量之间的关系。结果表明,①黄河入海口区的水沙通量有明显的季节性变化,其中沙通量的变化更为显著;②丰水年很少连续出现,枯水年有75%以连续两年的形式出现;③多沙年有连续几年出现1次的,也有连续2年或3年都出现的,少沙年基本上以连续形式出现,最多可达7年;④水沙通量间存在一定的相关性,其中细颗粒泥沙通量与水通量之间的相关性较弱。
Based on the observed data of runoff and sediment at the Lijin hydrological station in the period of 1950 - 2003, a statistical method is applied to study the seasonal and annual variations of runoff and sediment fluxes in the estuary. The results show that: (1) there is an obvious seasonal variation of runoff and sediment fluxes in the Yellow River Estuary, especially sediment flux; (2) the flood years seldom continuously appear and 75 % of the low-runoff years takes place in continuous two years; (3) the high sediment years appear once several years or continuous 2- 3 years, the low sediment years basically appear in continuous way even in 7 years; (4) there is a certain relationship between runoff and sediment fluxes, but the relationship between the fine grained sediment flux and runoff flux is poor.