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卢姁, 张东凌. 10月份热带印度洋海气耦合的统计动力诊断[J]. 大气科学, 2010, 34(2): 351-360. DOI: 10.3878/j.issn.1006-9895.2010.02.09
引用本文: 卢姁, 张东凌. 10月份热带印度洋海气耦合的统计动力诊断[J]. 大气科学, 2010, 34(2): 351-360. DOI: 10.3878/j.issn.1006-9895.2010.02.09
LU Xu, ZHANG Dongling. Dynamic Statistic Analysis of Coupled Circulation of Atmosphere and Ocean in the Tropical Indian Ocean in October[J]. Chinese Journal of Atmospheric Sciences, 2010, 34(2): 351-360. DOI: 10.3878/j.issn.1006-9895.2010.02.09
Citation: LU Xu, ZHANG Dongling. Dynamic Statistic Analysis of Coupled Circulation of Atmosphere and Ocean in the Tropical Indian Ocean in October[J]. Chinese Journal of Atmospheric Sciences, 2010, 34(2): 351-360. DOI: 10.3878/j.issn.1006-9895.2010.02.09

10月份热带印度洋海气耦合的统计动力诊断

Dynamic Statistic Analysis of Coupled Circulation of Atmosphere and Ocean in the Tropical Indian Ocean in October

  • 摘要: 本文将热带印度洋10月份的大气风场和海洋上层流场看作一个整体, 对其作了动力统计诊断, 即作了复EOF分析, 考察了其年际和年代际变化, 并揭示其与印度洋偶极子 (IOD) 和ENSO的关系。结果表明: 在同一模态中, 海洋模态表现出很强的赤道俘获现象, 而大气则无此现象; 第一模态为印度洋偶极子模态; 第二模态为ENSO前期在印度洋的延伸模态。前2个模态的风场都揭示了Walker环流异常的结构; 印度洋海温的年际变化主要取决于印度洋地区的海气耦合状态, 但太平洋的ENSO循环对其也有一定影响。

     

    Abstract: The Complex EOF (CEOF) analysis was carried out in order to study the interannual and interdecadal variations of the coupled circulation of atmosphere and ocean in the tropical Indian Ocean and unveil their relationship with the Indian Ocean dipole (IOD) and ENSO. The results show that: In the same mode, the anomalous current of ocean is equatorial-trapped, but the wind field has no such phenomena; the first mode has a close relationship with the IOD, the second mode counts much on ENSO; the atmosphere field of the first and second modes represents the abnormal changes of Walker circulation; the interannual variation of the Indian Ocean's temperature lies mainly on the coupled state of atmosphere and ocean about the Indian Ocean, but the ENSO circulation of the Pacific Ocean also has some influence.

     

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