[1]王玲玲,刘明元,李伟伟,等.黄土丘陵区小流域暴雨时空变化特征分析[J].水土保持研究,2010,17(01):225-227.
　WANG Ling-ling,LIU Ming-yuan,LI Wei-wei,et al.Characteristic Analysis of Rainstorm Temporal and Spatial Variability on Small Catchments in Loess Hilly Region[J].Research of Soil and Water Conservation,2010,17(01):225-227.
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黄土丘陵区小流域暴雨时空变化特征分析

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 17 期数: 2010年01期 页码: 225-227 栏目: 出版日期: 2010-02-20
Title:
Characteristic Analysis of Rainstorm Temporal and Spatial Variability on Small Catchments in Loess Hilly Region
作者:
王玲玲1,2, 刘明元3, 李伟伟4, 杨春霞1
1. 黄河水利科学研究院, 郑州, 450003;
2. 中国科学院水利部水土保持研究所, 黄土高原土壤侵蚀与旱地农业国家重点实验室, 陕西, 杨凌, 712100;
3. 新野县水利局, 河南, 新野, 473500;
4. 郑州大学环境技术咨询工程公司, 郑州, 450003
Author(s):
WANG Ling-ling1,2, LIU Ming-yuan3, LI Wei-wei4, YANG Chun-xia1
1. Yellow River Institute of Hydraulic, YRCC, Zhengzhou, 45003 China;
2. State Key Laboratory of Soil Erosion and Dry Land Farming on the Loess Plateau, Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling, Shanxi, 712100, China;
3. Water Conservancy Bureau of Xinye County, Xinye, He’nan, 473500, China
关键词:
暴雨; 时空分布; 小流域; 黄土丘陵区
Keywords:
rainstorm; temporal and spatial distribution; small watershed; Loess hilly region
分类号:
P426.616;P426.614
摘要:
了解黄土丘陵区暴雨时空变化特征,有利于深入研究土壤侵蚀机理.利用雨量站控制条件较好的桥沟小流域资料,统计分析了该流域30min、60min、120min和150min时段降雨及次降雨空间变化的关系,时段降雨分布同次降雨分布的内在联系以及次降雨的时空变化过程.结果表明,当分析时段达到一定长度以后,时段降雨对次降雨分布具有一定的代表性;降雨空间变化程度的相关距离关系随距离的增加而减弱,从时间上看,暴雨中心位置是不断变化的.
Abstract:
In order to better understand the temporal and spatial characteristics of rainstorm in loess hilly region,using small watershed data of Qiaogou,the relationship between 30 min,60 min,120 min,150 min period and rainfall were statistically analyzed.Furthermore,the temporal and spatial variations of rainfall and the intrinsically link between rainfall and period rainfall were studied.The results showed that when the period reaches a certain length,the rainfall is distributed fairly representatively by period rainfall;With the increasing of distance,the relativity of rainfall between rainfall stations weakened.With the change of time,the center location of rainstorm is constantly changing.All the results were useful to understand the mechanism of soil erosion further in-depth.

参考文献/References:

[1] 张汉雄.黄土高原的暴雨特性及其分布规律[J].地理学报,1983,38(4):416-425.
[2] 李长兴,沈晋,范荣生.黄土地区小流域降雨空间变化特征分析[J].水科学进展,1995,6(2):127-132.
[3] 焦菊英,王万中,郝小品.黄土高原不同类型暴雨的降水侵蚀特征[J].干旱区资源与环境,1999,13(1):34-42.
[4] 朱会义,贾绍凤.降雨信息空间插值的不确定性分析[J].地理科学进展,2004(2):35-43.
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备注/Memo

收稿日期:2008-8-16。
基金项目:水利部公益性行业科研专项(200701035);黄土高原土壤侵蚀与旱地农业国家重点实验室基金(10501－235)
作者简介:王玲玲:(1975- ),女,河南博爱人,硕士,从事土壤侵蚀与环境治理研究.E-mail:wlingling99@yahoo.com.cn

更新日期/Last Update: 1900-01-01