A CLASS OF HOMOTOPIC SOLVING METHOD FOR
ENSO MODEL
Mo Jiaqi;Lin Wantao;Wang Hui
【期刊名称】《数学物理学报（英文版）》 【年(卷),期】2009(029)001
【摘要】The E1 Nino/La Nina and the Southern Oscillation (ENSO) is an interannual phenomenon involved in the tropical Pacific ocean-atmosphere interactions. In this article, the aim is to create an asymptotic solving method of nonlinear equation for the ENSO models. And on the basis of a class of oscillator of ENSO models, using the method of homotopic mapping, the approximation of solution of corresponding problem is studied. It is proved from the results that homotopic method can be used for analyzing the SST anomaly in the equatorial eastern Pacific and the thermocline depth anomaly of the atmosphere-ocean oscillation for ENSO model. 【总页数】10页(101-110) 【关键词】
【作者】Mo Jiaqi;Lin Wantao;Wang Hui
【作者单位】Department of Mathemtics, Anhui Normal University, Wuhu 241000, China;Division of Computational Science, E-Institutes of Shanghai Universities at SJTU, Shanghai 200240, China;Department of Mathematics, Huzhou Teachers College, Huzhou 313000, China;LASG,
Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China;Chinese Academy of Meteorological Sciences, Beijing 100081, China 【正文语种】中文 【中图分类】O1 【相关文献】
1.Variational iteration solving method of a sea-air oscillator model for the ENSO [J], MO Jiaqi; LIN Wantao; WANG Hui
2.Idealized Experiments for Optimizing Model Parameters Using a 4D-Variational Method in an Intermediate Coupled Model of ENSO [J], Chuan GAO; Rong-Hua ZHANG; Xinrong WU; Jichang SUN
3.A CLASS OF TWO-STEP CONTINUITY RUNGE-KUTTA METHODS FOR SOLVING SINGULAR DELAY DIFFERENTIAL EQUATIONS AND ITS STABILITY ANALYSIS [J], Xin Leng; De-gui Liu; Xiao-qiu Song; Li-rong Chen
4.A Variational Iteration Solving Method for a Class of Generalized Boussinesq Equations [J], MO Jia-Qi
5.A class of fully third-order accurate projection methods for solving the incompressible Navier-Stokes equations [J], Yuxin Ren; Yuxi Jiang; Miao'er Liu; Hanxin Zhang
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A CLASS OF HOMOTOPIC SOLVING METHOD FOR ENSO MODEL
