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ID:28301730
大小:8.54 MB
页数:68页
时间:2018-12-09
《亚洲干旱半干旱区近几十年区域气候变化》由会员上传分享,免费在线阅读,更多相关内容在应用文档-天天文库。
1、兰州大学硕士学位论文亚洲干旱/半干旱区近几十年来气候变化摘要本文利用ERA-40年再分析资料分析了亚洲干旱/半干旱区气候特征、降水与大洋暖池气候的相关特征以及研究区的湿机制。结果表明:亚洲干旱/半干旱区剔除季节变化的水汽、降水与三个大洋暖池(WPWP、EIOWP和EP)区在南北纬loo之间区域水汽、海温都有非常显著的正相关关系。其中干旱/半干旱区降水与东印度洋暖池海温的相关性最好,与西太平洋暖池海温的相关性次之,与E1Ninol+2区的相关性较弱;E1Nino区越靠近中太平洋,亚洲干旱区与ElNino区水汽的相关性就越强。亚洲干旱/半
2、干旱区夏季的降水与EIOWPl、WPWPl/2和EP三个大洋暖池四季的海温都有较好的相关性;亚洲干旱/半干旱区的降水对EIOWPl的海温变化响应最快(降水变化延后海温变化1.3月),对WPWPl/2区海温变化的响应最慢(延迟4个月)。就季节尺度而言,在E1Nino年冬季和LaNina年的夏季,亚洲干旱/半干旱区的降水都比常年偏多。分析也表明,近年来由于西风减弱和印度季风的增强,使得更多的印度季风区和东亚季风区水汽被输送到亚洲干旱/半干旱区,是干旱区上空水汽增加,降水增多的原因之一。研究区高云覆盖近年来减弱,但是中、低云覆盖增加,表明低
3、层的辐合降水量增加;分析对流层顶层和低层的温度变化趋势发现,对流层低层温度升高,而顶层温度出现降低的趋势,这种温度的变化特征可以加剧对流层内大气的对流活动,有利于形成降水。我们还做了三个控制实验表明,如果海表温度(SST)增加,那么研究区上空的水汽就会随之而增加。关键词:亚洲干旱/半干旱区;大洋暖池;ENSO;水汽;降水;对流层顶层;云量覆盖;CCM3兰州大学硕士学位论文亚洲干旱/半干旱区近几十年来气候变化Abstract:UsingtheERA一40reanalysisdata,characteristicsofthecorrela
4、tionbetweentheprecipitationofAsianaridandsemiaridregionandtheoceanwarmpoolseasurfacetemperatures(SSTs),watervaporchangesareinvestigated.TheresultsshowthatthedeseasonalisedwatervaporandprecipitationinAsianaridandsemi-aridregionexhibitadistinctpositivecorrelationwithdesea
5、sonalisedSSTsandwatervaporOVertheoceanwarmpools.ThecorrelationismostsignificantintheEastIndianOceanWarmPool1(EIOWP1)andrelativelyweakinE1Ninol+2,butthecorrelationswithE1NinoregionsbecomestrongerwhenE1Ninoregionisclosertothecentrepacificregion.Thesummerprecipitationofthe
6、Asianaridandsemi—aridregioniswellcorrelatedwiththeoceanwarmpoolSSTsinallseasons.However,thewinterandspringprecipitationoftheAsianaridandsemi—aridregionhavenosignificantcorrelationwiththeoceanwarmpoolSSTs.ThequickestresponseoftheprecipitationintheAsianaridandsemi-aridreg
7、iontotheoceanwarmpoolSSTsisassociatedwithEIOWP1withatimelagof1-3months,andtheslowestresponsecorrespondstothewestpacificwarmpool(WPWP)withatimelagof4months.TheanalysisalsorevealsthattheprecipitationincreasesintheAsianaridandsemi-aridregiontendstoincreaseduringE1Ninoyearw
8、interandLaNinayearsummer.ThechangesinintensitiesoftheIndianMonsoon,EastAsianMonsoon,westerlyandENSOimpact,toal
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