干旱气象
榦旱氣象
간한기상
GANSU METEOROLOGY
2014年
1期
123-127
,共5页
白冰%陆登荣%陈学君%韩海涛%王有恒
白冰%陸登榮%陳學君%韓海濤%王有恆
백빙%륙등영%진학군%한해도%왕유항
兰州地区%降水量%正态分布%正态性检验
蘭州地區%降水量%正態分佈%正態性檢驗
란주지구%강수량%정태분포%정태성검험
Lanzhou region%precipitation%normal distribution%normality test
在对降水资料的分析过程中,要求资料的时间序列呈正态分布。利用兰州地区的兰州、皋兰、榆中和永登4个站点1960~2009年的降水量资料,采用“偏度-峰度系数+W检验”方法,基于SPSS软件,对兰州地区的年、季和月降水量正态特征进行分析。结果表明,兰州地区4个气象站的年降水量均呈正态性分布;兰州、皋兰和永登3站的夏、秋2季降水量为正态性分布,而榆中站只有秋季降水量为正态性分布,且秋季降水量的正态性最好,冬季最差;大多数月降水量不服从正态分布,但对降水序列进行平方根处理后,其正态性得到明显的改善。
在對降水資料的分析過程中,要求資料的時間序列呈正態分佈。利用蘭州地區的蘭州、皋蘭、榆中和永登4箇站點1960~2009年的降水量資料,採用“偏度-峰度繫數+W檢驗”方法,基于SPSS軟件,對蘭州地區的年、季和月降水量正態特徵進行分析。結果錶明,蘭州地區4箇氣象站的年降水量均呈正態性分佈;蘭州、皋蘭和永登3站的夏、鞦2季降水量為正態性分佈,而榆中站隻有鞦季降水量為正態性分佈,且鞦季降水量的正態性最好,鼕季最差;大多數月降水量不服從正態分佈,但對降水序列進行平方根處理後,其正態性得到明顯的改善。
재대강수자료적분석과정중,요구자료적시간서렬정정태분포。이용란주지구적란주、고란、유중화영등4개참점1960~2009년적강수량자료,채용“편도-봉도계수+W검험”방법,기우SPSS연건,대란주지구적년、계화월강수량정태특정진행분석。결과표명,란주지구4개기상참적년강수량균정정태성분포;란주、고란화영등3참적하、추2계강수량위정태성분포,이유중참지유추계강수량위정태성분포,차추계강수량적정태성최호,동계최차;대다수월강수량불복종정태분포,단대강수서렬진행평방근처리후,기정태성득도명현적개선。
It is generally known that the research on precipitation depends on normal distribution of the time-series data.Based on the observational precipitation data at 4 weather stations in Lanzhou,Gaolan,Yuzhong and Yongdeng of Lanzhou region from 1960 to 2009,the normality of the monthly,seasonal and annual precipitations were analyzed by using strictly the “skewness and sharpness coefficient +W test ”methods.The results showed that the annual precipitation of each station obeyed normal distribution in Lanzhou region.The seasonal precipitation in Lanzhou,Gaolan and Yongdeng was subject to normal distribution in summer and autumn,but that in Yuzhong was only subject to normal distribution in autumn,and the normality of precipitation in autumn was the best and the worst in winter in Yuzhong.In addition,most of the monthly precipitations at 4 stations didn’t conform normal distribution,however, the normality of their square root had been improved significantly.