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The results are as follows. Multiple time scale features can be seen in the whole seasonal and annual rainfall series. The 3~4 years period variations prevail in spring rainfall series, with a transition trend from 3 years period to 4 years period. 4 years and 14 years period variations are the main types in summer rainfall series. 2 years and 12 years period variations are mainly found in autumn rainfall series, and 4 years and 16 years period variations in winter rainfall sequence. 2 years, 4 years and 13 years period variations prevail in annual rainfall sequence. The sudden change of spring, winter and annual rainfall is not obvious. The mutation points of summer and autumn rainfall occur, respectively, in 1973 and 1963. The same tendency is seen in summer and annual rainfall sequence. The summer rainfall mutation influences the annual rainfall mutation. The rainfall of Shaoxing region will become affluent in the future 5~6 years according to the main period of summer and annual rainfall series., authors=null, authorsList=null, authorCompany=null, correspAuthors=null, authorNote=null, correspAuthorsNote=null, copyrightStatement=null, copyrightOwner=null, extLink=null, articleAbsUrl=null, sourceXml=null, magXml=null, pdfUrl=null, pdf=or87E/ECx84lCNm/TQz0pg==, pdfFileSize=1213351, pdfExtLink=null, richHtmlUrl=null, mobilePdfUrl=null, reviewReport=null, pdfFirstPage=null, abstractGraph=null, abstractGraphContent=null, abstractVideo=null, citation=null, cebUrl=null, magXmlContent=null, mapNumber=null, fund=null), CN=ArticleExt(id=1242117248383520821, articleId=1242117245908881438, tenantId=1146029695717560320, journalId=1146031591421210625, language=CN, title=绍兴市近48年降水演变特征统计分析, columnId=1146540929516700224, journalTitle=科技导报, columnName=研究论文, runingTitle=null, highlight=null, articleAbstract=选取绍兴国家气象观测站1961年1月至2009年2月逐月降水量作为降水分析基本资料,利用一元线性回归、小波变换和Mann-Kendall检验等统计学方法对绍兴降水季节变化和年际变化的特征进行了综合分析,分析了不同时间尺度下降水序列变化的周期和突变点,并根据主周期对未来降水变化趋势进行了预估。结果发现,绍兴市近48 a各个季节和年降水都存在多时间尺度特征,大尺度的周期变化中嵌套有小尺度的周期变化。春季降水以3~4 a年周期为主,并有准3 a周期向准4 a周期转变的趋势;夏季降水主要存在准4 a和准14 a周期变化;秋季降水主要存在准2 a和准12 a周期变化;冬季降水主要存在准4 a和准16 a周期变化;年降水主要存在准2 a和准4 a年际周期变化和准13 a年代际周期变化。绍兴春季和冬季降水突变不明显;夏季和秋季突变明显,突变点分别出现在1973年和1963年,而年降水突变不明显,不存在明显的突变期。夏季降水变化趋势和年降水趋势基本一致;夏季降水和年降水在时域上分布有很大的相似性,都具有准4 a周期变化,并全时域存在;夏季降水突变影响到全年降水的突变。根据绍兴夏季降水和年降水的主周期推测,2009年后的5~6 a绍兴年降水将相对偏多。, authors=庞盛荣,罗国军, authorsList=庞盛荣;罗国军, authorCompany=上虞市气象局, correspAuthors=null, authorNote=null, correspAuthorsNote=庞盛荣, copyrightStatement=null, copyrightOwner=null, extLink=null, articleAbsUrl=null, sourceXml=null, magXml=null, pdfUrl=null, pdf=gPHS3xcVhoUc8BGMV+xFsQ==, pdfFileSize=1213351, pdfExtLink=null, richHtmlUrl=null, mobilePdfUrl=null, reviewReport=null, pdfFirstPage=null, abstractGraph=null, abstractGraphContent=null, abstractVideo=null, 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绍兴市近48年降水演变特征统计分析
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绍兴市近48年降水演变特征统计分析
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庞盛荣,罗国军
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    上虞市气象局
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庞盛荣
Statistical Analysis of 48 Year's Rainfall in Shaoxing
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    出版时间: 2009-09-28
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    选取绍兴国家气象观测站1961年1月至2009年2月逐月降水量作为降水分析基本资料,利用一元线性回归、小波变换和Mann-Kendall检验等统计学方法对绍兴降水季节变化和年际变化的特征进行了综合分析,分析了不同时间尺度下降水序列变化的周期和突变点,并根据主周期对未来降水变化趋势进行了预估。结果发现,绍兴市近48 a各个季节和年降水都存在多时间尺度特征,大尺度的周期变化中嵌套有小尺度的周期变化。春季降水以3~4 a年周期为主,并有准3 a周期向准4 a周期转变的趋势;夏季降水主要存在准4 a和准14 a周期变化;秋季降水主要存在准2 a和准12 a周期变化;冬季降水主要存在准4 a和准16 a周期变化;年降水主要存在准2 a和准4 a年际周期变化和准13 a年代际周期变化。绍兴春季和冬季降水突变不明显;夏季和秋季突变明显,突变点分别出现在1973年和1963年,而年降水突变不明显,不存在明显的突变期。夏季降水变化趋势和年降水趋势基本一致;夏季降水和年降水在时域上分布有很大的相似性,都具有准4 a周期变化,并全时域存在;夏季降水突变影响到全年降水的突变。根据绍兴夏季降水和年降水的主周期推测,2009年后的5~6 a绍兴年降水将相对偏多。
    降水演变  /  小波分析  /  Mann-Kendall检验  /  多时间尺度
    This paper analyzes the historical rainfall data of Shaoxing National Meteorological Observatory, by using methods of linear regression, wavelet analysis and Mann-Kendall mutation testing, to reveal the seasonal variation and interannual change of 48 year's rainfall series in Shaoxing region., and to forecast the future rainfall. The results are as follows. Multiple time scale features can be seen in the whole seasonal and annual rainfall series. The 3~4 years period variations prevail in spring rainfall series, with a transition trend from 3 years period to 4 years period. 4 years and 14 years period variations are the main types in summer rainfall series. 2 years and 12 years period variations are mainly found in autumn rainfall series, and 4 years and 16 years period variations in winter rainfall sequence. 2 years, 4 years and 13 years period variations prevail in annual rainfall sequence. The sudden change of spring, winter and annual rainfall is not obvious. The mutation points of summer and autumn rainfall occur, respectively, in 1973 and 1963. The same tendency is seen in summer and annual rainfall sequence. The summer rainfall mutation influences the annual rainfall mutation. The rainfall of Shaoxing region will become affluent in the future 5~6 years according to the main period of summer and annual rainfall series.
    rainfall evolution  /  wavelet analysis  /  Mann-Kendall mutation testing  /  multiple time scales
    庞盛荣;罗国军. 绍兴市近48年降水演变特征统计分析. 科技导报, 2009 , 27 (0918) : 60 -65 .
    . Statistical Analysis of 48 Year's Rainfall in Shaoxing[J]. Science & Technology Review, 2009 , 27 (0918) : 60 -65 .

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    鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
    小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
    多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
    红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
    小菇属 Mycena 11 5.26
    光柄菇属 Pluteus 5 2.39
    红菇属 Russula 17 8.13
    栓菌属 Trametes 5 2.39
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