全部 标题 作者
关键词 摘要

OALib Journal期刊
ISSN: 2333-9721
费用:99美元

查看量下载量

相关文章

更多...
地理学报  2011 

近50年来淮河流域极端降水的时空变化及统计特征

DOI: 10.11821/xb201109005, PP. 1200-1210

Keywords: 淮河,极端降水,L-矩法,K-S检验

Full-Text   Cite this paper   Add to My Lib

Abstract:

以淮河流域27个气象站点1960-2009年逐日降水观测资料为基础,选取年最大降水量序列(AM)和超门限峰值序列(POT),分析淮河流域年极端降水事件的时空变化趋势,研究淮河流域降水极值的统计特征。研究发现过去50年,淮河流域大多数站点年最大日降水量有增加的趋势,少数站点有减少的趋势,但增加和减少的趋势均不明显。从单个气象站点50年降水序列来看,年最大日降水事件发生的时间大多集中于20世纪60-70年代,且以汛期居多。利用L-矩法、K-S检验等方法,发现GEV和GP分布分别能够较好的拟合AM和POT序列。通过计算比较在不同重现期水平下的降水量,发现POT序列及其对应的GP分布能够更好的模拟淮河流域极端降水序列。

References

[1]  HuHaoran,MaoXiaoliang,LiangLing.TemporalandspatialvariationsofextremeprecipitationeventsoffloodseasonoverSichuanBasininlast50years.ActaGeographicaSinca,2009,64(3):278-288.[胡豪然,毛晓亮,梁玲.近50年四川盆地汛期极端降水事件的时空演变.地理学报,2009,64(3):278-288.]
[2]  CaiMin,DingYuguo,JiangZhihong.ExtremeprecipitationexperimentationovereasternChinabasedonL-momentestimation.PlateauMeteorology,2007,26(2):309-318.[蔡敏,丁裕国,江志红.我国东部极端降水时空分布及其概率特征.高原气象,2007,26(2):309-318.]
[3]  LiuXuefeng,XiangLiang,YuChangwen.CharacteristicsoftemporalandspatialvariationsoftheprecipitationextremesintheHaiheRiverBasin.ClimaticandEnvironmentalResearch,2010,15(4):451-461.[刘学锋,向亮,于长文.海河流域降水极值的时空演变特征.气候与环境研究,2010,15(4):451-461.]
[4]  ZhaiPanmao,PanXiaohua.ChangeinextremetemperatureandprecipitationovernorthernChinaduringthesecondhalfofthe20thcentury.ActaGeographicaSinica,2003,58(增刊):1-10.[翟盘茂,潘晓华.中国北方近50年温度和降水极端事件变化.地理学报,2003,58(增刊):1-10.]
[5]  SuBuda,GemmerMarco,JiangTongetal.ProbabilitydistributionofprecipitationextremesovertheYangtzeRiverbasinduring1960-2005.AdvancesinClimateChangeResearch,2007,3(4):208-213.[苏布达,GemmerM,姜彤等.1960-2005年长江流域降水极值慨率分布特征.气候变化研究进展,2007,3(4):208-213.]
[6]  XiaoHui,JiangAijun,ShenZhenetal.Thespace-timedistributioncharactersofmaximumdiurnalprecipitationinJiangsuProvinceandthestatisticassimilation.ScientiaMeteorologicaSinica,2006,26(2):177-182.[肖卉,姜爱军,沈填等.江苏省最大日降水量时空分布特征及其统计拟合.气象科学,2006,26(2):177-182.]
[7]  DongQuan,ChenXing,ChenTiexietal.RelationshipbetweenextremesofprecipitationanddischargeintheHuaiheRiverBasin.JournalofNanjingUniversity:NaturalScience,2009,45(6):790-801.[董全,陈星,陈铁喜等.淮河流域极端降水与极端流量关系的研究.南京大学学报:自然科学版,2009,45(6):790-801.]
[8]  GroismanPY,KarlTR,EasterlingDRetal.Changesintheprobabilityofheavyprecipitation:Importantindicatorsofclimaticchange.ClimaticChange,1999,42(1):243-283.
[9]  DingYuguo,JiangZhihong.TheIntroductionofExtremeClimateResearch.Beijing:ChinaMeteorologicalPress,2009.[丁裕国,江志红.极端气候研究方法导论.北京:气象出版社,2009.]
[10]  XuZongxue.Long-termtrendofprecipitationintheYellowRiverBasinduringthepast50years.GeographicalResearch,2006,25(1):27-34.[徐宗学.黄河流域近50年降水变化趋势分析.地理研究,2006,25(1):27-34.]
[11]  ChuJianting,XiaJun,XuChongyuetal.Comparisonandspatial-temporalvariabilityofdailyprecipitationdataofweatherstationsandraingaugesinHaiheRiverbasin.ActaGeographicaSinca,2009,64(9):1083-1092.[褚健婷,夏军,许崇育等.海河流域气象和水文降水资料对比分析及时空变异.地理学报,2009,64(9):1083-1092.]
[12]  ZhangQiang,LiJianfeng,ChenXiaohongetal.SpatialvariabilityofprobabilitydistributionofextremeprecipitationinXinjiang.ActaGeographicaSinca,2011,66(1):3-12.[张强,李剑锋,陈晓宏等.基于Copula函数的新疆极端降水概率时空变化特征.地理学报,2011,66(1):3-12.]
[13]  IPCC.Climatechange2007:Thephysicalsciencebasis//ContributionofWorkingGroupItotheFourthAssessmentReportoftheIntergovernmentalPanelonClimateChange.Cambridge:CambridgeUniversityPress:2007.
[14]  WangFang,TianHong.CharacteristicsofextremeprecipitationeventsinHuaiheRiverBasinin1960-2007.AdvancesinClimateChangeResearch,2010,6(3):228-229.[汪方,田红.淮河流域1960-2007年极端强降水事件特征.气候变化研究进展,2010,6(3):228-229.]
[15]  ZhangTing.ProbabilitydistributionofprecipitationextremesduringrainingseasonsinSouthChina.ActaMeteorologicaSinica,2009,67(3):442-450.[张婷.华南地区汛期极端降水的概率分布特征.气象学报,2009,67(3):442-450.]
[16]  ZhangJinling,WangJi.TemporalandspatialvariationcharacteristicofextremeprecipitationeventsintheYangtzeandHuaiheriverbasinofChinafrom1961to2006.JournalofAnhuiAgriculturalSciences,2009,37(7):3089-3091.[张金玲,王冀.1961-2006年江淮流域极端降水事件变化特征.安徽农业科学,2009,37(7):3089-3091.]
[17]  MaXiaoqun,ChenXiaoyi,YaoYun.SpatialandtemporalchangesofprecipitationatdifferentgradesandtheirimpactsonagricaltureinHuaiheRiverBasinofAnhuiProvince.ChineseJournalofAgrometeorology,2009,30(1):25-30.[马晓群,陈晓艺,姚筠.安徽淮河流域各级降水时空变化及其对农业的影响.中国农业气象,2009,30(1):25-30.]
[18]  WeiFengying,ZhangTing.OscillationcharacteristicsofsummerprecipitationintheHuaiheRivervalleyandrelevantclimatebackground.ScienceinChina:SeriesD,2009,39(10):1360-1374.[魏凤英,张婷.淮河流域夏季降水的振荡特征及其与气候背景的联系.中国科学:D辑,2009,39(10):1360-1374.]
[19]  WijngaardJB,KleinTankAMG,KonnenGP.Homogeneityof20thcenturyEuropeandailytemperatureandprecipitationseries.InternationalJournalofClimatology,2003,23(6):679-692.
[20]  SuBuda.ProbabilisticcharacteristicsofprecipitationextremesovertheYangtzeRiverbasin.ScientiaMeteorologicaSinica,2008,28(6):625-629.[苏布达.长江流域极端强降水分布特征的统计拟合.气象科学,2008,28(6):625-629.]
[21]  YueS,WangCY.ApplicabilityofprewhiteningtoeliminatetheinfluenceofserialcorrelationontheMann-Kendalltest.WaterResourcesResearch,2002,38(6),doi:10.1029/2001WR000861.
[22]  HoskingJRM,WallisJR.RegionalFrequencyAnalysis.Cambridge:CambridgeUniversityPress,1997.
[23]  HoskingJRM.L-moments:Analysisandestimationofdistributionsusinglinearcombinationsoforderstatistics.JournaloftheRoyalStatisticalSociety:SeriesB(Methodological),1990,52(1):105-124.
[24]  CaiMin.AdvantagesofL-momentestimationanditsapplicationtoextremeprecipitation.ScientiaMeteorologicaSinica,2007,27(6):597-603.[蔡敏.L-矩估计方法在极端降水研究中的应用.气象科学,2007,27(6):597-603.]
[25]  XiongLihua,GuoShenglian.ApplicationofL-momentsintheregionalfloodfrequencyanalysis.WaterPower,2003,29(3):6-8.[熊立华,郭生练.L-矩在区域洪水频率分析中的应用.水力发电,2003,29(3):6-8.]

Full-Text

Contact Us

service@oalib.com

QQ:3279437679

WhatsApp +8615387084133