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简易海洋同化数据中的厄尔尼诺现象

崔茂常 吴玲娟

崔茂常, 吴玲娟. 简易海洋同化数据中的厄尔尼诺现象[J]. 海洋学报, 2005, 27(2): 29-38.
引用本文: 崔茂常, 吴玲娟. 简易海洋同化数据中的厄尔尼诺现象[J]. 海洋学报, 2005, 27(2): 29-38.
CUI Mao-chang, WU Ling-juan. El Niño phenomenon in SODA data[J]. Haiyang Xuebao, 2005, 27(2): 29-38.
Citation: CUI Mao-chang, WU Ling-juan. El Niño phenomenon in SODA data[J]. Haiyang Xuebao, 2005, 27(2): 29-38.

简易海洋同化数据中的厄尔尼诺现象

基金项目: 国家“863”计划项目(2001AA633060);中国科学院海洋研究所知识创新工程项目(L370221117)

El Niño phenomenon in SODA data

  • 摘要: 为研究在厄尔尼诺现象演变过程中海气相互作用的性态特征,该文再次应用拓展伴随模态分析于简易海洋同化数据(SODA data).结果表明:通过相互作用形成厄尔尼诺/拉尼娜现象的海洋与大气具有明显不同的性态,气候系统中并不存在一个相对独立的热带太平洋大气变异,但是的确存在一个相对独立的热带太平洋海洋变异;原因在于大气是底部界面受热而海洋是顶部界面受热,从而导致前者具有较后者强烈得多的斜压不稳定性和能够覆盖大部分热带太平洋的赤道辐合带; 再次证实了正是直接来自中纬度海域的西风爆发和海面风辐聚导致赤道太平洋上层海水的东向移动和经向辐聚造就了厄尔尼诺所特有的增温信号.
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出版历程
  • 收稿日期:  2004-08-12
  • 修回日期:  2005-01-10

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