| 西太平洋副高的东西进退与东亚夏季风系统的相互影响与关联 |
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| 引用本文： | 余丹丹,;张韧,;赵越超,;万雷,;郭小璇.西太平洋副高的东西进退与东亚夏季风系统的相互影响与关联[J].南京气象学院学报,2014(3):304-312. |
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| 作者姓名： | 余丹丹 ;张韧 ;赵越超 ;万雷 ;郭小璇 |
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| 作者单位： | [1]北京5111信箱,北京100094; [2]解放军理工大学气象海洋学院,江苏南京211101; [3]南京信息工程大学滨江学院,江苏南京210044 |
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| 基金项目： | 国家自然科学基金资助项目（41075045） |
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| 摘 要： | 利用1980-2010年NCEP/NCAR再分析资料和美国NOAA向外长波辐射（outgoing longwave radiation,OLR）资料,根据关键区500 hPa位势高度的变化定义了西太平洋副高东西位置指标,利用该指标围绕东亚夏季风系统开展分析,详细对比了夏季6月、7月副高东西向活动异常时,季风区相应的环流及对流活动差异.结果表明：副高东西位置的年际变化反映了亚洲夏季风的强弱变化,副高偏西（东）年,南海夏季风偏弱（强）,副热带夏季风偏强（弱）;副高的东西进退与东亚夏季风系统成员之间相互影响、相互制约;副高偏西年,南亚高压偏东、偏强,季风槽不发展、强度偏弱,西风带长波槽发展加深,南半球马斯克林高压和澳大利亚高压减弱,越赤道气流减弱,而副高偏东年情况则反之.
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| 关 键 词： | 副热带高压 东亚夏季风 相互影响 |
Correlation between the subtropical high abnormal longitudinal position and the East Asian summer monsoon system |
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| Institution: | YU Dan-dan ,ZHANG Ren ,ZHAO Yue-chao ,WAN Lei, GUO Xiao-xuan ( 1.P.O. Box 5111 ,Beijing 100094,China; 2.College of Meteorology and Oceanography, PLA University of Science and Technology, Nanjing 211101, China; 3.Binjiang School,NUIST,Nanjing 210044,China) |
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| Abstract: | Using the NCEP/NCAR reanalysis data and the OLR （outgoing longwave radiation） data from NOAA during 1980-2010,an index is defined to describe the longitudinal position of the western Pacific subtropical high based on 500 hPa potential height variation in the key areas.With the index,an investigation is carded out closely with the East Asian summer monsoon system,and the circulation and convective activity differences are revealed in the monsoon area as the subtropical high position is abnormal in June and July.Results show that the abnormal eastern-western position of the subtropical high reflects the Asian summer monsoon intensity,that is,when the subtropical high position is west（east）,the South China Sea＇s summer monsoon is weak（strong）,and the subtropics summer monsoon is strong （weak）.There exists some interaction between the advance and retreat of the subtropical high and members of the East Asia monsoon system.In the western subtropical high years,the South Asia high is strong with eastern position,the monsoon trough is weaker,the long-wave trough develops deeper,the Mascarene high and the Australia high is weaker,and the cross-equatorial flow is also weaker.The situation is contrary in the eastern subtropical high years. |
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| Keywords: | subtropical high East Asian summer monsoon interaction |
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