2007
DOI: 10.1088/1009-1963/16/3/003
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Asymptotic solution of a sea–air oscillator for ENSO mechanism

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Cited by 13 publications
(6 citation statements)
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“…By operating integrating factor and substituting the conditions: T(0) = 0, h(0) =0, τ 1 (0) = 0, τ 2 (0) = 0 given in [10] into (21)-(24), the following solutions can easily be obtained: Next, on applying (25)-(28) into the equations (17)-(20) respectively, the restof the components of the iteration formulae can be reached with the aid of the Maple computer algebra package where the first-order approximate solution of the variational iteration method are computed as below:…”
Section: Variational Iteration Methodsmentioning
confidence: 99%
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“…By operating integrating factor and substituting the conditions: T(0) = 0, h(0) =0, τ 1 (0) = 0, τ 2 (0) = 0 given in [10] into (21)-(24), the following solutions can easily be obtained: Next, on applying (25)-(28) into the equations (17)-(20) respectively, the restof the components of the iteration formulae can be reached with the aid of the Maple computer algebra package where the first-order approximate solution of the variational iteration method are computed as below:…”
Section: Variational Iteration Methodsmentioning
confidence: 99%
“…The positive ocean-atmosphere feedback or coupled ocean-atmosphere instability contributes to a continuously warm equatorial Pacific region. Now, we consider the sea-air oscillator of the ENSO model presented in [10]:…”
Section: Introductionmentioning
confidence: 99%
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“…Approximate methods have been developed and improved, including the method of averaging, the boundary layer method, the matched asymptotic expansion method, and the multiple scales method (Dawes and Proctor, 2008;Graef and Kong, 2008;Hovhannisyan and Vulanovic, 2008;Ramos, 2009). Using the perturbation method, Mo et al studied some of nolinear perturbation problems (Mo et al, 2004;2007a;2007b;Mo and Wang, 2007;Mo and Lin, 2008a;2008b;2008c;Mo, 2009a;2009b;2009c). In this paper, we discuss a model of the thermally and wind-driven ocean circulation and obtain an approximate solution of the model by using the homotopic mapping perturbation method.…”
Section: Introductionmentioning
confidence: 99%
“…Recently, many scholars have done a great deal of work (Ni and Wei, 2006;Khasminskii and Yin, 2005;Marques, 2005;Bobkova, 2005). Using the differential inequalities and other methods, Mo et al (2003) also provided a class of shock layer solution of nonlinear equations for the singularly perturbed problems and the E1 Ni o phenomenon of atmospheric physics (Mo et al, 2004;2006;2007). In this paper, using a special singular perturbation method, we study interhemispheric THC model in atmosphere-ocean for global climate.…”
Section: Introductionmentioning
confidence: 99%