Lam函数和非线性演化方程的扰动方法

利用小扰动方法对非线性演化方程作展开得到原始方程的各级近似方程 .应用Jacobi椭圆函数展开法求得了零级近似方程的准确解 ,并由此得到一级近似方程和二级近似方程分别满足齐次Lam 方程和非齐次Lam 方程 ,应用Lam 函数和Jacobi椭圆函数展开法可以分别求得一级近似方程和二级近似方程的准确解 .这样 ,就求得了非线性演化方程的多级准确解 .     

Lamé函数和非线性演化方程的扰动方法

利用小扰动方法对非线性演化方程作展开得到原始方程的各级近似方程.应用Jacobi椭圆函数展开法求得了零级近似方程的准确解,并由此得到一级近似方程和二级近似方程分别满足齐次Lamé方程和非齐次Lamé方程,应用Lamé函数和Jacobi椭圆函数展开法可以分别求得一级近似方程和二级近似方程的准确解.这样,就求得了非线性演化方程的多级准确解.     

一类非线性演化方程的新多级准确解

在Lamé方程和新的Lamé函数的基础上，应用小扰动方法和Jacobi椭圆函数展开法求解一类非线性演化方程（如mKdV方程，非线性Klein-Gordon方程Ⅱ等），获得多种新的多级准确解 .这些多级准确解对应着不同形式的周期波解.这些解在极限条件下可以退化为多种形式的孤 立波解，如带状孤立子、钟形孤立子等. 关键词： Jacobi椭圆函数 Lam函数 多级准确解 非线性演化方程 扰动方法     

NONLINEAR WAVES IN GEOPHYSICAL FLUID

In this paper, beginning with the shallow-water equations describing the geophysical fluid motion and by a method expanding the nonlinear terms in Taylor series near the equilibrium point, we find the analytic solutions of the finite amplitude nonlinear inertio-surface gravity waves and Rossby waves. We point out that (ⅰ) the finite amplitude nonlinear inertio-surface gravity waves and Rossby waves Satisfy all the KdV equations; (ⅱ) the solutions are all the enoidal functions, i. e. the enoidal waves which include the linear waves and form the solitary waves under certain conditions; (ⅲ) the dispersive relation including both the wave number and the amplitude is established; (ⅳ) the rotating transform method is given, and the two-dimensional nonlinear problem can be reduced to the one-dimensional one.     

求某些非线性偏微分方程特解的一个简洁方法

简单介绍了应用一个简洁的“试探函数法”求解非线性偏微分方程的基本步骤,主要研究了两大类方程,一类是Burgers方程或KdV方程的推广,另一类是具有特殊非线性反应率的Fisher方程.不难看出,这个方法是简洁的,并且可望进一步扩展.     

New exact solutions to KdV equations with variable coefficients or forcing

Jacobi elliptic function expansion method is extended to construct the exact solutions to another kind of KdV equations, which have variable coefficients or forcing terms. And new periodic solutions obtained by this method can be reduced to the soliton-typed solutions under the limited condition.     

NONLINEAR ROSSBY WAVES FORCED BY TOPOGRAPHY

Using a barotropic semi-geostrophic model with topographic forcing the stability and solutions of the nonlinear Rossby waves are discussed. It is found that the effects of the W-E oriented topography and the N-S oriented topography on the stability and phase speed of the waves are quite different. It is also found that the nonlinear Rossby waves forced by the topography can be described by the well-known KdV equation.     

地球物理流体中的非线性Rossby波

本文利用半地转近似和运行波方法研究了地球物理流体(大气和海洋)中的非线性Rossby波,它们满足KdV方程.     

一类厄尔尼诺一南方涛动充电-放电振子模型研究

通过数学变换将一类厄尔尼诺．南方涛动（简称ENSO）的充电．放电振子模型转换成vanderPol方程,由vanderPol方程的定性分析严格证明了该ENSO振荡子模型存在一个稳定的极限环．     

间歇湍流的分数阶动力学

间歇湍流意味着湍流涡旋并不充满空间,其维数介于2和3之间.湍流扩散为超扩散,且概率密度分布具有长尾特征.本文将流体力学的Navier-Stokes(NS)方程中的黏性项用分数阶的拉普拉斯算子表达.分析表明,分数阶拉普拉斯的阶数α和间歇湍流的维数D相联系.对于均匀各向同性的Kolmogorov湍流α=2,即用整数阶NS方程描述.而对于间歇性湍流,一定用分数阶的NS方程来描述.对于Kolmogorov湍流,扩散方差正比于t3,即Richardson扩散.而对于间歇性湍流,扩散方差要比Richardson扩散更强.