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Variational iteration solving method for El Nino phenomenon atmospheric physics of nonlinear model

机译:非线性模型的厄尔尼诺现象大气物理学的变分迭代求解方法

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摘要

A class of El Nifio atmospheric physics oscillation model is considered. The El Nino atmospheric physics oscillation is an abnormal phenomenon involved in the tropical Pacific ocean-atmosphere interactions. The conceptual oscillator model should consider the variations of both the eastern and western Pacific anomaly patterns. An El Nino atmospheric physics model is proposed using a method for the variational iteration theory. Using the variational iteration method, the approximate expansions of the solution of corresponding problem are constructed. That is, firstly, introducing a set of functional and accounting their variationals, the Lagrange multiplicators are counted, and then the variational iteration is defined, finally, the approximate solution is obtained. From approximate expansions of the solution, the zonal sea surface temperature anomaly in the equatorial eastern Pacific and the thermocline depth anomaly of the sea-air oscillation for El Nino atmospheric physics model can be analyzed. El Nino is a very complicated natural phenomenon. Hence basic models need to be reduced for the sea-air oscillator and are solved. The variational iteration is a simple and valid approximate method.
机译:考虑了一类厄尔尼诺现象的大气物理学振荡模型。厄尔尼诺现象的大气物理学振荡是一种异常现象,涉及热带太平洋海-气相互作用。概念性震荡器模型应考虑东部和西部太平洋异常模式的变化。利用变分迭代理论的方法,提出了一个El Nino大气物理模型。使用变分迭代法,构造了相应问题解的近似展开式。也就是说,首先引入一组函数并考虑它们的变分,对拉格朗日乘数进行计数,然后定义变分迭代,最后获得近似解。从解的近似展开,可以分析厄尔尼诺现象的物理模型在赤道东太平洋的纬向海表温度异常和海气振荡的温跃层深度异常。厄尔尼诺现象是非常复杂的自然现象。因此,需要简化海气振荡器的基本模型并加以解决。变分迭代是一种简单有效的近似方法。

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