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从实测径流看华北地区水资源
引用本文:李桂忱,马振骅.从实测径流看华北地区水资源[J].高原气象,1999,18(4):613-617.
作者姓名:李桂忱  马振骅
作者单位:中国科学院大气物理研究所,北京,100029
基金项目:中国科学院“九·五”重大应用基础研究项目
摘    要:简述了华北地区主要河流水系(滦河、海河、黄河中下游)地表水的现状,地重要径流控制站的年均径流量作了年代际的统计分析。结果表明:降水随年代际有升有降,径流也随着降水的起伏而变化,但是径流与降水的区别在于70年代之后充随年代际的递减趋势十分明显。

关 键 词:径流  年代际

WATER RESOURCE IN NORTH CHINA DEDUCED FROM MEASURED RUNOFF
LI Gui-chen,MA Zhen-hua.WATER RESOURCE IN NORTH CHINA DEDUCED FROM MEASURED RUNOFF[J].Plateau Meteorology,1999,18(4):613-617.
Authors:LI Gui-chen  MA Zhen-hua
Abstract:The present situation of ground surface water of main river systems,in North China,such as Luanhe river,Haihe river,and middle and lower reaches of Yellow River,is simply described. The inter decade statistical analysis of yearly averaged runoff in some important runoff control stations is made. The important result is,as rainfall rises and falls as decade passes,runoff undulates just as rainfall. The difference is that the runoff has an obvious decreasing tendency decade by decade since 1970's.
Keywords:Runoff  Inter  decade
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