| 纬向平均副热带高压和Hadley环流下沉支的关系 |
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| 引用本文： | 吴国雄,刘屹岷,刘平,任荣彩. 纬向平均副热带高压和Hadley环流下沉支的关系[J]. 气象学报, 2002, 60(5): 635-636 |
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| 作者姓名： | 吴国雄 刘屹岷 刘平 任荣彩 |
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| 作者单位： | 中国科学院大气物理研究所,LASG,北京,100029 |
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| 基金项目： | 国家自然科学基金委项目 ( 4 0 135 0 2 0、4990 5 0 0 2和 40 0 2 30 0 1)。 |
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| 摘 要： | 气象学者传统地认为副热带高压带是Ｈａｄｌｅｙ环流的下沉支形成的。鉴于冬 (夏 )季Ｈａｄｌｅｙ环流最强 (弱 )时副热带高压反而最 (弱 )强的事实 ,Ｈｏｓｋｉｎｓ[1] 对经典理论提出质疑。吴国雄等[2 ,3] 指出副热带高压 (下文中称副高 )的形成主要是加热的垂直非均匀造成的。刘屹岷等[4 ,5] 发现夏季 5 0 0ｈＰａ月平均图上 165°Ｅ以西的西太平洋副高以上升运动为特征。一般来说 ,受副高控制天气晴好 ,这与西太平洋副高以上升运动为特征是否有矛盾。为此 ,我们首先研究气候纬向平均副高的动力问题 ,结果表明Ｈａｄｌｅｙ环流和副高形成…
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| 收稿时间： | 2002-07-25 |
| 修稿时间： | 2002-07-25 |
RELATION BETWEEN THE ZONAL MEAN SUBTROPICAL ANTICYCLONE AND THE SINKING ARM OF THE HADLEY CELL |
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| Wu Guoxiong,Liu Yimin,Liu Ping and Ren Rongcai. RELATION BETWEEN THE ZONAL MEAN SUBTROPICAL ANTICYCLONE AND THE SINKING ARM OF THE HADLEY CELL[J]. Acta Meteorologica Sinica, 2002, 60(5): 635-636 |
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| Authors: | Wu Guoxiong Liu Yimin Liu Ping Ren Rongcai |
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| Affiliation: | State Key Laboratory of Numerical Modelling for AtmosphericSciences and Geophysical Fluid Dynamics(LASG) Institute of Atmospheric Physics, Chinese Academy of Science, Beijing 100029;State Key Laboratory of Numerical Modelling for AtmosphericSciences and Geophysical Fluid Dynamics(LASG) Institute of Atmospheric Physics, Chinese Academy of Science, Beijing 100029;State Key Laboratory of Numerical Modelling for AtmosphericSciences and Geophysical Fluid Dynamics(LASG) Institute of Atmospheric Physics, Chinese Academy of Science, Beijing 100029;State Key Laboratory of Numerical Modelling for AtmosphericSciences and Geophysical Fluid Dynamics(LASG) Institute of Atmospheric Physics, Chinese Academy of Science, Beijing 100029 |
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