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[1]LUO Han,JIA Hui-hui,ZHAO Ting-ning,et al.Study on the Spatial Distribution Pattern of the Rainfall in the Loess Region of West Shaanxi——A Case Study in Tuqiaogou Small Watershed in Fangshan of Shaanxi Province[J].Research of Soil and Water Conservation,2010,17(04):180-182,187.

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Study on the Spatial Distribution Pattern of the Rainfall in the Loess Region of West Shaanxi——A Case Study in Tuqiaogou Small Watershed in Fangshan of Shaanxi Province

Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume: 17 Number of periods: 2010 04 Page number: 180-182,187 Column: Public date: 2010-08-20

Title:: Study on the Spatial Distribution Pattern of the Rainfall in the Loess Region of West Shaanxi——A Case Study in Tuqiaogou Small Watershed in Fangshan of Shaanxi Province

Author(s):: LUO Han, JIA Hui-hui, ZHAO Ting-ning, DONG Mei; Key Laboratory of Soil and Water Conservation and Desertification Combating of Ministry of Education, College of Soil and Water Conservation, Beijing Forestry University, Beijing 100083, China

Keywords:: loess hill and gully region region; rainfall; distribution pattern

CLC:: P426.615

DOI:: -

Abstract:: The rainfall is the direct source of water resources on land,especially in the rainfall deficient loess area.Through the research for rainfall spatial distribution,we can provide the instruction for the planted forest cultivation,the vegetation restoration,and the research on soil erosion.Through the rainfall scope on different terrain position,we carried on the rainfall observation.In view of different altitude and slope to the rainfall measured data contrastive analysis,the conclusion was drawn in this paper.The rainfall increases at first,then reduces along with the altitude,and the most rainfall occurred nearby the altitude of 1 280m.The patterns of the rainfall distribution along with the slope aspects followed the order of leeward slope>against the wind slope,namely the shady slope>the sunny slope,and the rainfall occurred in the loess hill was moderate.

References:: [1] 姚丽华.气象学[M].北京:中国林业出版社,1992.
[2] 袁嘉祖.华北地区山坡小气候与造林成活率[C]//山地气候文集编委会.山地气候文集.北京:气象出版社,1984.
[3] 徐学选,张北赢,琚彤军.黄土丘陵区降雨、径流、土壤水分的时空分布与利用对策[J].生态环境,2005,14(6):890-893.
[4] 傅抱璞.山地气候研究的若干问题[C]//山地气候文集编委会.山地气候文集.北京:气象出版社,1984.
[5] 何红艳,郭志华,肖文发.降水空间插值技术的研究进展[J].生态学杂志,2005,24(10):1187-1191.
[6] 樊述全.鄱阳湖流域降雨时空分布规律及其水文响应[D].南京:河海大学,2007.
[7] 李丽娟,王娟,李海滨.无定河流域降雨量空间变异性研究[J].地理研究,2002,2I(4):434-439.
[8] 袁世琼.流域平均降雨量计算方法的探讨[J].四川水利,1987(4):4-13.
[9] 傅抱璞.山地气候[M].北京:科学出版社,1987.
[10] 孙鹏森,刘世荣,李崇巍.基于地形和主风向效应模拟山区降水空间分布[J].生态学报,2004,24(9):1910-1915.
[11] 苏宏新,桑卫国.山地小气候模拟研究进展[J].植物生态学报,2002,26(增刊):107-114.

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