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弱频散条件下大气运动的非线性演变过程
引用本文:薛纪善,郭秉荣.弱频散条件下大气运动的非线性演变过程[J].气象学报,1993,51(2):248-252.
作者姓名:薛纪善  郭秉荣
作者单位:广东省热带海洋气象研究所,武汉大学数学系 广州 510080,430072
摘    要:研究非线性过程对大气运动影响的一个常用方法是在一定条件下,将大气运动力学方程化为一些熟知的典型非线性演变方程,再利用数学中已有的结果进行讨论。Long、Redekopp等从地转涡度方程出发,证明了迭加在带状切变气流中的长的Rossby波的演变可以用著名的Kdv方程来描述。此

收稿时间:1989/9/26 0:00:00
修稿时间:1991/10/27 0:00:00

NONLINEAR EVOLUTION OF WEAKLY-DISPERSIVE ATMOSPHERIC MOTIONS
Xue Jishan and Guo Bingrong.NONLINEAR EVOLUTION OF WEAKLY-DISPERSIVE ATMOSPHERIC MOTIONS[J].Acta Meteorologica Sinica,1993,51(2):248-252.
Authors:Xue Jishan and Guo Bingrong
Institution:Guangdong Inttitute of Tropical Marine Meteorology, Guangzhou 510080;Department of Mathematics, Wuhan University, 430072
Abstract:Based on conservative equation of potential vorticity,it is proved that the atmospheric nonlinear evolution in weak frequency-dispersion condition is usually governed by KdV equation and the forms of weak frequency-dispersion conditionsare discussed.Sonm prvious researches on derivation of KdV equation from different specified atmospheric motions are actually the special cases of the general form in this paper.The KdV equation can be resolved by numerical method.The resulte present that the initial disturbance in limited domain will develop the isolated wave under one given condition and a series of frequency-dispersing waves under other given conditions.
Keywords:
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