气象与环境科学
氣象與環境科學
기상여배경과학
METEOROLOGICAL AND ENVIRONMENTAL SCIENCES
2011年
3期
56-60
,共5页
降水%时空演变特征%季节变化
降水%時空縯變特徵%季節變化
강수%시공연변특정%계절변화
precipitation%time-space evolution feature%seasonal variety
利用河南省110个观测站1965-2009年降水数据,采用空间分析和时间序列分析相结合的方法,对河南省年降水和四季降水以及不同降水界限的年代变化进行了时空演变特征分析并进行了0.05的显著性检验,结果表明:近45 a河南省年降水呈弱上升趋势,不同降水界限范围具有较明显的年际变化特征。从时间分布上看,春季与冬季变化趋势相似,都呈弱增加趋势;夏季呈显著增加趋势;秋季呈显著减少趋势。从空间分布上看,春季安阳西北部降水增多趋势显著,其他地区无论是降水增多或是减少均不显著;夏季全省大部地区降水增多,其中周口和平顶山两地区降水增多趋势显著;秋季大部地区为降水减少趋势,其中南阳、信阳两地区降水减少显著;冬季,全省大部分地区降水增多,但增多趋势不显著。
利用河南省110箇觀測站1965-2009年降水數據,採用空間分析和時間序列分析相結閤的方法,對河南省年降水和四季降水以及不同降水界限的年代變化進行瞭時空縯變特徵分析併進行瞭0.05的顯著性檢驗,結果錶明:近45 a河南省年降水呈弱上升趨勢,不同降水界限範圍具有較明顯的年際變化特徵。從時間分佈上看,春季與鼕季變化趨勢相似,都呈弱增加趨勢;夏季呈顯著增加趨勢;鞦季呈顯著減少趨勢。從空間分佈上看,春季安暘西北部降水增多趨勢顯著,其他地區無論是降水增多或是減少均不顯著;夏季全省大部地區降水增多,其中週口和平頂山兩地區降水增多趨勢顯著;鞦季大部地區為降水減少趨勢,其中南暘、信暘兩地區降水減少顯著;鼕季,全省大部分地區降水增多,但增多趨勢不顯著。
이용하남성110개관측참1965-2009년강수수거,채용공간분석화시간서렬분석상결합적방법,대하남성년강수화사계강수이급불동강수계한적년대변화진행료시공연변특정분석병진행료0.05적현저성검험,결과표명:근45 a하남성년강수정약상승추세,불동강수계한범위구유교명현적년제변화특정。종시간분포상간,춘계여동계변화추세상사,도정약증가추세;하계정현저증가추세;추계정현저감소추세。종공간분포상간,춘계안양서북부강수증다추세현저,기타지구무론시강수증다혹시감소균불현저;하계전성대부지구강수증다,기중주구화평정산량지구강수증다추세현저;추계대부지구위강수감소추세,기중남양、신양량지구강수감소현저;동계,전성대부분지구강수증다,단증다추세불현저。
By using precipitation data of 110 observation stations in Henan f rom 1965 to 2009,combing with spatial analysis and time series analysis,the ti me-space evolution feature of annual precipitation,seasonal precipitation and a nnual variety of different precipitation boundary was analyzed,the 0.05 test of significance was made at the same time.The results showed that the annual prec ipitation had a weak anabatic trend and the annual variety feature of different precipitation boundary was obvious.From the view of temporal distribution,the trends were similar in spring and in winter,which were weak enhancive trends.W hile they were distinct increase and decrease in summer and autumn respectively. From the view of spatial distribution,in spring,the precipitation trend was n either distinct increase nor decrease except in northwestward of Anyang in where the trend was distinct increase.In summer,precipitation of most places increa sed especially in Zhoukou and Pingdingshan.On the contrary,in autumn,precipit ation of most places decreased especially in Nanyang and Xinyang.In winter,the trend was increased but not distinct.