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通道建立的内在本质还说善始善终的最优化论环境梯度和波导环境的波动与传播多样性

已有 415 次阅读 2023-4-29 08:15 |系统分类:观点评述

引子  临界面确立   通道构建    临界隶属    选择机制  通道维护   能信流    临界不完备  全息仿真

一、多节点尺度规模临界扩张算法取义

       上边界的内波源由压力随机特性的内波生成共振理论解释。因扰动源在表面产生一个移动的压力场,当压力场的对流速度及其在同一方向上的波数与某一内波的波数和频率满足共振条件时,内波即被激发,涉及风压和垂向流影响下的内波增长。内部主要源于破碎及斜压不稳定导致的内部大尺度环流和中尺度涡的串级衰减过程。以上总体涉及地形边界起伏下表面应力、压力分布、震源扰动、引潮诱导的涡-波-流-固相互作用,但均受地转与内部连续分异调控。 

二、理性之光的情感附带

     In a nonlinear theory, the determination of the ground state is nontrivial. The assumption of stationarity is to some degree arbitrary and requires justification. Indeed, in experiments, large scale motion is regarded as a background phenomenon, but the mutual interaction of such motions may give rise to nonlinear effects of infinite intensity.

三、不可为的完备性差异

     The nonlinear evolution process can be interpreted as the dynamics of the interaction of waves of different types. The only restriction on the suggested wave classification system is that the measurement time must be shorter than the time of accumulation of nonlinear effects. It should be noted that projection operators are useful in the linear theory as well. They allow one to distinguish the relations between dynamical variables of a given wave type under the initial conditions in their simplest form.

四、正则运算的无欲而刚

       Every measurement system used for identification can be correlated (as in quantum mechanics) with the projection operator onto the subspace of a given dispersion branch.Mathematical description of this operator follows naturally from the language used to describe dispersion relations, i.e., from a linearized system of equations. The solution of the linear system has been elaborated and the system of eigenvectors for the matrix of the Hermitian evolution operator is complete. The relations between the components of the eigenvectors are treated as polarization equations which need to be found. It is important to stress that the form of the evolution operator depends on the formulation of the problem.

五、胁迫分异的构造诱导与时间配置

      Sound waves, internal waves, and Rossby waves are related to such classes of waves in geophysical dynamics, as are Kelvin, Lamb, and Poincaré waves.This rather simple classification is based on a linearized model that assumes an exponential dependence of the basic equations on height. The system is transformed to one with constant coefficients that admits Fourier transform to the k domain.Determination of wave type according to frequency is not sufficient for complete identification because the frequency (wavelength) intervals can overlap.




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