海河流域典型山区子流域近34年气候及径流变化趋势  

Variance Tendency of Precipitation and Runoff in Mountain Watershed of Hai River Basin in Recent 34 Years

作　　者：田菲[1,2] 韩淑敏[1] 胡玉昆 

机构地区：[1]中国科学院遗传与发育生物学研究所农业资源研究中心,石家庄050021 [2]中国科学院研究生院,北京100039 [3]河北省水利科学研究院,石家庄050021

出　　处：《中国农业气象》2009年第1期60-65,共6页Chinese Journal of Agrometeorology

基　　金：中国科学院知识创新工程重要方向项目(KZCX3-SW-446);中科院"百人计划项目"

摘　　要：基于海河流域27个气象站点和7个子流域出水口的水文站点34a(1966-1999年)逐日观测气象水文数据,运用非参数统计检验方法(Mann-Kendall法)对滹沱河、冶河、洋河、桑干河、唐河、沙河、潮白河7个典型山区子流域的气候和径流变化趋势及时空分布进行分析。结果表明:(1)降雨量呈下降趋势的测站较多,占66.67%,但大部分都没有通过0.05水平的检验,下降趋势不明显。(2)气温呈上升趋势的测站较多,占88.89%,且大部分测站都通过了0.05水平的显著性检验,上升趋势明显。(3)径流量普遍呈下降趋势,但程度各不相同,南部和西北部流域下降趋势明显(通过了0.05水平的检验),其它子流域不明显。Based on the daily meteorological and hydrological data of 27 meteorological stations and 7 hydrological stations in the outlet of the region from 1966 to 1999, the spatiotemporal distribution of precipitation and runoff in seven typical mountain watershed such as Hutuo river, Ye river, Yang river, Sanggan river, Tang river, Sha river and Chaobai river of the Hai River Basin were analyzed with the Mann-Kendall test method. The results indicated that the precipitation was not significantly decreased in the most meteorological stations, which took 66.67% , while the temperature was significantly increased in the most meteorological stations, which took 88.89%. The runoff experienced great decrease, but the downward degree was not the same. It significantly decreased in the South and Northwest Parts.

关 键 词：降雨 温度 径流 海河流域 MANN-KENDALL 

分 类 号：S162[农业科学—农业气象学]