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Ensemble Simulations of a Nonlinear Barotropic Model for the North Atlantic Oscillation  
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【英文篇名】 Ensemble Simulations of a Nonlinear Barotropic Model for the North Atlantic Oscillation
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【英文作者】 ZHANG Dong-Bin 1; 2; JIN Fei-Fei 3; LI Jian-Ping 1; and DING Rui-Qiang 1 1 State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics (LASG); Institute of Atmospheric Physics; Chinese Academy of Sciences; Beijing 100029; China 2 Graduate University of Chinese Academy of Sciences; Beijing 100049; China 3 Department of Meteorology; University of Hawaii at Manoa; Honolulu; Hi 96822; USAd;
【文献出处】 Atmospheric and Oceanic Science Letters , 大气和海洋科学快报(英文版), 编辑部邮箱 2010年 05期  
期刊荣誉:ASPT来源刊  CJFD收录刊
【英文关键词】 ensemble-mean; NAO; nonlinearity;
【摘要】 A numerical ensemble-mean approach was employed to solve a nonlinear barotropic model with stochastic basic flows to analyze the nonlinear effects in the formation of the North Atlantic Oscillation (NAO). The nonlinear response to external forcing was more similar to the NAO mode than the linear response was, indicating the importance of nonlinearity. With increasing external forcing and enhanced low-frequency anomalies, the effect of nonlinearity increased. Therefore, for strong NAO events, nonlinearity sh...
【英文摘要】 A numerical ensemble-mean approach was employed to solve a nonlinear barotropic model with stochastic basic flows to analyze the nonlinear effects in the formation of the North Atlantic Oscillation (NAO). The nonlinear response to external forcing was more similar to the NAO mode than the linear response was, indicating the importance of nonlinearity. With increasing external forcing and enhanced low-frequency anomalies, the effect of nonlinearity increased. Therefore, for strong NAO events, nonlinearity sh...
【基金】 supported by the National Basic Research Program of China (973 program) (Grant No. 2010CB950400) ; the National Natural Science Foundation of China (NSFC) (Grant Nos. 41030961 and 40805022)
【更新日期】 2011-10-17
【分类号】 P732
【正文快照】 1 Introduction The North Atlantic Oscillation (NAO) is a prominent mode of the general atmospheric circulation in the North- ern Hemisphere during the winter (Walker and Bliss, 1932; Wallace and Gutzler, 1981) and can be considered part of the global-scal

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天文学、地球科学
  海洋学
   海洋基础科学
    海洋气象学
  
 
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