灾害性天气预报理论模式的稳定性分析

详细讨论、分析了涉及灾害性天气预报的理论模式的稳定性,这些模式包括:非静力完全弹性方程组、滞弹性方程组．证明了非静力完全弹性方程组在无穷可微函数类中是稳定方程;滞弹性方程组则因为对流体的特殊假设,改变了连续方程的形式,于是出现了“流体为粘性与不可压假设的匹配”现象,从而使在实际预报工作中占有重要地位的这一类重要方程组与Navier-Stokes方程呈现了相同拓扑性质的不稳定性,而这是在数值预报工作中首先应该避免的．据此提出了如何修改应用模式的参考意见．     

大气运动基本方程组的稳定性分析

以分层理论提供的基本方法分析大气运动基本方程组的拓扑学特征;证明局地直角坐标系中的大气运动基本方程组在无穷可微函数类中是稳定方程;给出局部解意义下使方程组典型定解问题适定的充要条件;讨论大气动力学中有关“以过去推测未来”以及当涉及应用问题时如何修改定解条件和下垫面的选择等问题;指出在通常假设下,基本方程组中的3个运动方程和连续方程完全决定了这个方程组的性质．     

Navier-Stokes方程与Euler方程的稳定性比较

比较了Navier-Stokes 方程和Euler方程的稳定性;并以它们的典型初值问题为例,分析了Navier-Stokes方程和Euler方程稳定性不同的原因．     

大尺度湿大气原始方程组对边界参数的连续依赖性

大气的大尺度动力学方程由Navier-Stokes方程导出的原始方程组控制,并与热力学和盐度扩散输运方程耦合.在过去的几十年里,人们从数学的角度对大气、海洋与耦合了大气和海洋的原始方程组进行了广泛的研究.许多学者的研究主要关注原始方程组在数学上的逻辑性,即方程组的适定性.笔者开始注意到研究原始方程组自身稳定性的必要性.因为在模型建立、简化的过程中不可避免地会出现一些误差,这就需要研究方程组中系数的微小变化是否会引起方程组解的巨大变化.该文运用原始方程组解的先验估计,结合能量估计与微分不等式技术,展示了如何控制水汽比,证明了大尺度湿大气原始方程组的解对边界参数的连续依赖性.     

平面不可压缩的NAVIER-STOKES方程新五模类LORENZ方程组的混沌行为

本文研究了平面正方形区域上不可压缩的Navier-Stokes方程五模类Lorenz方程组的混沌行为问题.利用傅立叶展开方法对Navier-Stokes方程进行模式截断,获得了新五模类Lorenz方程组,给出了该方程组定常解及其稳定性的讨论,证明了该方程组吸引子的存在性,并对其全局稳定性进行了分析和讨论.     

关于一类广义Navier-Stokes方程的稳定性

应用分层理论,通过证明所论方程是l-简单的,l≥1,证明了其不稳定性.以大气动力学中的强迫耗散非线性系统方程组解的不唯一性,作为这一结果的例证.     

Navier-Stokes方程五模类Lorenz方程组的动力学行为及数值仿真

本文对平面正方形区域上不可压缩的Navier-Stokes方程,进行傅立叶展开后,截断得到五模类Lorenz方程组.给出了该方程组定常解及其稳定性的讨论,证明了该方程组吸引子的存在性,并对其全局稳定性进行了分析和讨论,数值模拟了雷诺数在一定范围内变化时,类Lorenz方程组的动力学行为.     

简化Navier-Stokes方程的一般理论

本文研究简化Navier-Stokes方程的一般形式及数学物理背景。所提出的张量型简化方程能够适应一般固壁情况,且具有最大的简化效果。文中运用主次特征法并结合力学背景,阐明了简化方程的影响域和决定域,为相应数值方法提供基本依据。还通过对流扩散过程的细致分析,表明流场中扩散效应具有顺着流动方向的影响域,向流动上游的传播十分有限;Reynolds准则的倒数表征粘性效应向流动上游的传播距离、以及顺流方向粘性效应与垂直流动方向粘性效应的相对强弱;从而说明了较大Reynolds数下完全Navier-Stokes方程向简化Navier-Stokes方程的自然转化,并将简化的概念推广于传热传质。     

同心球间旋转流动类Lorenz方程组的分歧问题

本文对同心球间旋转流动的Navier-Stokes方程谱展开后进行三模态截断,研究了所得到的类Lorenz型方程组的分歧问题.推导了同心球间旋转流动的Navier-Stokes方程的流函数-涡度形式,给出了静态奇异点的条件,并计算出解分支.     

完整Coriolis力作用下的非线性近惯性波

从包含有完整Coriolis力作用下的大气运动原始基本方程组出发,通过尺度分析,采用多重尺度法及摄动展开法,推导了中高纬大气非线性近惯性波振幅演化所满足的Korteweg-de Vries方程.从演化方程的结果可以看出Coriolis参数水平分量对非线性近惯性波的影响,主要体现为对频散效应的修正及与基本流的相互作用.从理论上解释了完整Coriolis力作用下的中高纬地区大气非线性近惯性波运动的物理机制.     

Navier-Stokes方程稳定性研究(Ⅲ)

本文给出Navier-Stokes方程某些初值问题存在C2解的必要条件,并给出其在{t=0}上的初值问题不适定的例证。Navier-Stokes方程的初值问题是研究这个方程的基础问题之一。国内外很多学者在这方面的研究曾取得了不同程度的结果。法国时J.Leray教授就曾在某种意义下证明过Navier-Stokes方程某种初边值问题解的存在性[3].本文根据J.Hadamard的偏微分方程的基础理论[1].给出某些关键问题的严格定义,叙述一个有关Navipr-Stokes方程不稳定的基本定理。最后给出若干例证,其证明可参见[4].     

两个非同心旋转圆柱间粘性流动的广义雷诺方程及其基本流

运用张量分析方法及修正双极坐标系,建立了轴承润滑流动所应满足的广义Reynolds方程.应用薄流层中的Navier-Stokes方程的渐近分析方法和张量分析工具,得到了两个非同心旋转圆柱之间粘性流动的基本流所应满足的方程.这个基本流可以表示为两个同心旋转圆柱之间的Taylor流加上一个扰动项,并且给出了数值计算例子.     

Stretching and Shrinking of the Loop Soliton Interacting with a External Field

The integrable equation of motion of the loop soliton interacting with an external field is considered from the standpoint of stretching and/or shrinking of the loop. To study the role of the elastic force and the nonlinear forces, the basic equation is divided into three equations. We obtain stationary solutions for these equations and numerically solve their initial value problems to seek stability of the loop soliton.     

Strong solutions to the equations of a ferrofluid flow model

We study the differential system introduced by M.I. Shliomis to describe the motion of a ferrofluid driven by an external magnetic field. The system is a combination of the Navier-Stokes equations, the magnetization equation and the magnetostatic equations. No regularizing term is added to the magnetization equation. We prove the local-in-time existence of strong solutions to the system.     

Instability in the critical case of pair of pure imaginary roots for a class of systems with aftereffect

The stability of a system described by Volterra integrodifferential equations is investigated in the critical case when the characteristic equation has a pair of pure imaginery roots. Conditions for instability, analogous to the well-known conditions from the theory of differential equations [1], are derived. (A similar result was established previously in [2] for integrodifferential equations of simpler structure with integral kernels of exponential-polynomial type). For the proof, several manipulations are used to simplify the original equation and, in particular, to reduce the linearized equation to the form of a differential equation with constant diagonal matrix. (An analogous approach was used to analyse instability for Volterra integrodifferential equations in the critical case of zero root in [3, 4]). As an example, the sign of the Lyapunov constant in the problem of the rotational motion of a rigid body with viscoelastic supports is calculated.     

Stability analysis of the plane Couette flow for a model kinetic equation

The stability of the plane Couette flow is studied using the simplified Boltzmann equation (the BGK equation) in which the high modes in the space of velocities and coordinates are truncated. The solution to the Navier-Stokes equation with small additional terms depending on the Knudsen number is used as the stationary solution. We assume that the perturbations depend only on the coordinate that is orthogonal to the flow. The density perturbations are assumed to be nonzero. In this approximation, the problem is found to be unstable in the case of small Knudsen numbers.     

Convergence Rate to Stationary Solutions for Boltzmann Equation with External Force

For the Boltzmann equation with an external force in the form of the gradient of a potential function in space variable, the stability of its stationary solutions as local Maxwellians was studied by S. Ukai et al. (2005) through the energy method. Based on this stability analysis and some techniques on analyzing the convergence rates to stationary solutions for the compressible Navier-Stokes equations, in this paper, we study the convergence rate to the above stationary solutions for the Boltzmann equation which is a fundamental equation in statistical physics for non-equilibrium rarefied gas. By combining the dissipation from the viscosity and heat conductivity on the fluid components and the dissipation on the non-fluid component through the celebrated H-theorem, a convergence rate of the same order as the one for the compressible Navier-Stokes is obtained by constructing some energy functionals.