Temporal and Spatial Characteristics of Dry and Wet Conditions in Shiyang River Basin during the Period of 1960-2009

Jun-ju Zhou, Peiji Shi
{"title":"Temporal and Spatial Characteristics of Dry and Wet Conditions in Shiyang River Basin during the Period of 1960-2009","authors":"Jun-ju Zhou, Peiji Shi","doi":"10.1109/ICMULT.2010.5631420","DOIUrl":null,"url":null,"abstract":"Based on the climatic data of four meteorological stations from 1960 to 2009,using FAO Penman-Monteith model, ArcGIS IDW interpolation and Mann-Kendall test and T-test, the paper analyzes the changing trends,spatial and temporal differences and mutation characteristics of surface dry and wet conditions.The results show: Firstly, the overall trend of surface dry and wet conditions had been becoming wetter and wetter with the trend rate of humid index 0.006/10yr during the period of 1960-2009 in Shiyang River Basin.The surface was drier in the period of 1960s-1970s,and then became wetter after 1980s,especially after 2000.Secondly,the spatial differences of surface dry and wet conditions are significant.The mean annual humid index decreased from 0.404 of the upper reaches to 0.081 of the lower reaches gradually and the changing rates also changed from fast to slow. Furthermore, the lower reaches appeared the most dramatic fluctuation, followed by the upper reaches and the slightest fluctuation in the middle of river.Thirdly,the seasonal variations of surface dry/wet conditions were very different.The mean annual humid index was the largest in summer,followed by the autumn and the less in winter and spring.The overall changing trends of four seasons were all increasing,but the wetting trend was more significant in autumn and winter than that in spring and summer.Correlation analysis shows the correlation coefficients between summer, autumn,winter,spring and the mean annual were 0.665,0.591,0.397 and 0.334 respectively,which were all accepted for the 1% significance level,indicating the humid index increasing in the four seasons,especially for the two fomers, made greater contribution to the annual humid index changing.Finally,the mutation threshold of annual humid index occurred in the year around 1983,while the mutation years for the winter,spring and autunm were 1984,1981 and 1999 respectively and the unconspicuous mutation in summer.","PeriodicalId":412601,"journal":{"name":"2010 International Conference on Multimedia Technology","volume":"41 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2010-11-11","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"2010 International Conference on Multimedia Technology","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1109/ICMULT.2010.5631420","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0

Abstract

Based on the climatic data of four meteorological stations from 1960 to 2009,using FAO Penman-Monteith model, ArcGIS IDW interpolation and Mann-Kendall test and T-test, the paper analyzes the changing trends,spatial and temporal differences and mutation characteristics of surface dry and wet conditions.The results show: Firstly, the overall trend of surface dry and wet conditions had been becoming wetter and wetter with the trend rate of humid index 0.006/10yr during the period of 1960-2009 in Shiyang River Basin.The surface was drier in the period of 1960s-1970s,and then became wetter after 1980s,especially after 2000.Secondly,the spatial differences of surface dry and wet conditions are significant.The mean annual humid index decreased from 0.404 of the upper reaches to 0.081 of the lower reaches gradually and the changing rates also changed from fast to slow. Furthermore, the lower reaches appeared the most dramatic fluctuation, followed by the upper reaches and the slightest fluctuation in the middle of river.Thirdly,the seasonal variations of surface dry/wet conditions were very different.The mean annual humid index was the largest in summer,followed by the autumn and the less in winter and spring.The overall changing trends of four seasons were all increasing,but the wetting trend was more significant in autumn and winter than that in spring and summer.Correlation analysis shows the correlation coefficients between summer, autumn,winter,spring and the mean annual were 0.665,0.591,0.397 and 0.334 respectively,which were all accepted for the 1% significance level,indicating the humid index increasing in the four seasons,especially for the two fomers, made greater contribution to the annual humid index changing.Finally,the mutation threshold of annual humid index occurred in the year around 1983,while the mutation years for the winter,spring and autunm were 1984,1981 and 1999 respectively and the unconspicuous mutation in summer.
1960-2009年石羊河流域干湿条件时空特征
基于1960 - 2009年4个气象站的气候资料,利用FAO Penman-Monteith模型、ArcGIS IDW插值、Mann-Kendall检验和t检验,分析了地表干湿条件的变化趋势、时空差异和突变特征。结果表明:①1960—2009年石羊河流域地表干湿状况总体呈湿润化趋势,湿润指数趋势率为0.006/10yr;20世纪60 ~ 70年代地表较为干燥,80年代以后,特别是2000年以后,地表较为湿润。其次,地表干湿状况的空间差异显著。年平均湿度指数从上游的0.404逐渐下降到下游的0.081,变化速率也由快到慢。下游波动幅度最大,上游次之,中游波动幅度最小。③地表干湿条件的季节变化差异较大。年平均湿度指数以夏季最大,秋季次之,冬春季次之。四季总体变化趋势均呈增加趋势,但秋季和冬季湿润趋势较春季和夏季更为显著。相关分析显示,夏季、秋季、冬季、春季与年平均的相关系数分别为0.665、0.591、0.397和0.334,均为1%显著水平,说明四季湿润指数的增加对年湿润指数变化的贡献更大,尤其是冬季和春季。年湿润指数的突变阈值出现在1983年左右,冬季、春季和秋季的突变年份分别为1984年、1981年和1999年,夏季突变不显著。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
自引率
0.00%
发文量
0
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:604180095
Book学术官方微信