Shear flow energy redistribution stipulated by the internal-gravity wavy structures in the dissipative ionosphere

The linear mechanism of generation, intensification and further nonlinear dynamics of internal gravity waves (IGW) in stably stratified dissipative ionosphere with non-uniform zonal wind (shear flow) is studied. In case of the shear flows the operators of linear problem are non-selfadjoint, and the corresponding Eigen functions – nonorthogonal. Thus, canonical – modal approach is of less use studying such motions. Non-modal mathematical analysis becomes more adequate for such problems. On the basis of non-modal approach, the equations of dynamics and the energy transfer of IGW disturbances in the ionosphere with a shear flow is obtained. Exact analytical solutions of the linear as well as the nonlinear dynamic equations of the problem are built. The increment of shear instability of IGW is defined. It is revealed that the transient amplification of IGW disturbances due time does not flow exponentially, but in algebraic – power law manner. The effectiveness of the linear amplification mechanism of IGW at interaction with non-uniform zonal wind is analyzed. It is shown that at initial linear stage of evolution IGW effectively temporarily draws energy from the shear flow significantly increasing (by an order of magnitude) own amplitude and energy. With amplitude growth the nonlinear mechanism turns on and the process ends with self-organization of nonlinear solitary, strongly localized IGW vortex structures (the monopole vortex, the transverse vortex chain or the longitudinal vortex street). Accumulation of these vortices in the ionospheric medium can create the strongly turbulent state.     

Prediction of nonlinear pilot-induced oscillation using an intelligent human pilot model

This paper proposes a method to predict nonlinear Pilot-Induced Oscillation (PIO) using an intelligent human pilot model. This method is based on a scalogram-based PIO metric, which uses wavelet transforms to analyze the nonlinear characteristics of a time-varying system. The intelligent human pilot model includes three modules: perception module, decision and adaptive module, and execution module. Intelligent and adaptive features, including a neural network receptor, fuzzy decision and adaptation, are also introduced into the human pilot model to describe the behavior of the human pilot accommodating the nonlinear events. Furthermore, an algorithm is proposed to describe the procedure of the PIO prediction method with nonlinear evaluation cases. The prediction results obtained by numerical simulation are compared with the assessments of flight test data to validate the utility of the method. The flight test data were generated in the evaluation of the Smart-Cue/Smart-Gain, which is capable of reducing the PIO tendencies considerably. The results show that the method can be applied to predict the nonlinear PIO events by human pilot model simulation.     

Accuracy analysis of GNSS-IR snow depth inversion algorithms

In recent years, with the continuous development of Global Navigation Satellite System (GNSS), it has been applied not only to navigation and positioning, but also to Earth surface environment monitoring. At present, when performing GNSS-IR (GNSS Interferometric Reflectometry) snow depth inversion, Lomb-Scargle Periodogram (LSP) spectrum analysis is mainly used to calculate the vertical height from the antenna phase center to the reflection surface. However, it has the problem of low identification of power spectrum analysis, which may lead to frequency leakage. Therefore, Fast Fourier Transform (FFT) spectrum analysis and Nonlinear Least Square Fitting (NLSF) are introduced to calculate the vertical height in this paper. The GNSS-IR snow depth inversion experiment is carried out by using the observation data of P351 station in PBO (Plate Boundary Observatory) network of the United States from 2013 to 2016. Three algorithms are used to invert the snow depth and compared with the actual snow depth provided by the station 490 in the SNOTEL network. The observations data of L1 and L2 bands are respectively used to find the optimal combination between different algorithms further to improve the accuracy of GNSS-IR snow depth inversion. For L1 band, different snow depths correspond to different optimal algorithms. When the snow depth is less than 0.8 m, the inversion accuracy of NLSF algorithm is the highest. When the snow depth is greater than 0.8 m, the inversion accuracy of FFT algorithm is higher. Therefore, according to the different snow depth, a combined algorithm of NLSF + FFT is proposed for GNSS-IR snow depth inversion. Compared with the traditional LSP algorithm, the inversion accuracy of the combined algorithm is improved by 10%. For L2 band data, the results show that the accuracy of snow depth inversion of various algorithms do not change with the variations of snow depth. Among the three single algorithms, the inversion accuracy of FFT algorithm is better than that of LSP and NLSF algorithms.     

模糊控制方法及其在飞控中的应用

对于较大的飞行包线，飞机对象的参数变化剧烈，采用常规控制方法往往不能保证在较大飞行包线范围内均取得良好的控制效果，基于此，提出了一种新型的自组织模糊控制方法，该对系统内部参数的剧烈变化具有很强的适应性，然后对飞机飞行控制系统的控制律设计进行了研究。用所提出的模糊控制方法设计了部分控制律，最后以某型国产飞机对象，采用飞机六自由度非线性仿真模型，在一个较大的飞行包线范围内，进行了飞行仿真，取得了良好的     

一种非线性规划的求解方法与燃气发生器的设计

阐述了一种新的非线性规划的求解方法。即对每个参变量在其可能变化区间内，按照特定的步长依次代入约束方程来观察是否满足约束条件，从而求得若干组可行解。变量变化的步长通过非线性方程组各个方程在近似结点的全微分的分析获得。步长的确定是本方法的关键。文中并示范性列举了本方法在燃气发生器设计中的作用。     

非线性解耦控制与飞机敏捷性机动

首先介绍了以微分几何控制理论为基础的非线性系统解耦理论，给出了解耦控制律的综合方法及解耦闭环系统平衡点的计算方法，并对解耦系统的稳定性进行分析，随后用非线性解耦理论研究了飞机非线性运动的三种解耦运动模式，并讨论了飞机非线性解耦控制规律的线性近似解，最后用飞机非线性运动的三种解耦运动模式实现了三种形式的敏捷性机动，结果是满意的。为飞机敏捷性，直接力控制和过失速机动问题提供了一种理论研究方法。     

三维球坐标系下重力波波包非线性传播过程听数值研究

采用全隐欧拉（FICE）格式，对三维球坐标系下重力波波包在中层大气的非线性传播过程进行了数值模拟，模拟结果完整地反映了重力波波包在中层大气的非线性传播过程，并与线性重力波理论进行了定量比较。     

行波管非线性失真和交调干扰分析及其软件实现

行波管功率放大器(TWTA)是卫星通信星载系统中重要的高功放元件,TWTA的非线性特性会使多载波信号产生交调成份,导致交调失真、邻道干扰,影响通信系统的性能。通过建立基于TWTA的AM-AM与AM-PM效应的非线性模型,采用V isual C 6.0,开发了可根据TWTA参数动态建立非线性模型并能对任意载波信号产生的交调干扰进行分析的软件,对实际应用具有一定价值。     

一种基于量测方程线性变换的 GPS 定位算法

提出一种将ＧＰＳ导航中的量测方程线性化的方法,即是将直接法的方程降阶法应用于ＧＰＳ导航定位的量测方程中,计算机模拟结果表明此线性变化法可靠,实用。     

中层大气受迫 Rossby 波包的非线性相互作用Ⅰ.理论分析

本文研究了中层大气受迫Rossby波包非线性三波相互作用问题。理论分析得出,如果仅有最大波长或最小波长的波包受外源作用,系统仅能维持受迫波包的运动,平衡状态下外源能量不向另两个波包传递;仅有中等波长波包受外源作用时,随着外源强度的增加,系统的平衡态会发生分岔,并且在分岔点以后,中等波长波包的波幅不再增大,但大气高度愈高该振幅饱和值愈大,外源增大的能量全部通过非线性相互作用馈送给其他两个波包,从而外源可以维持三个波包的长期等幅运动。本文还给出了系统中有两个受迫Rossby波包时系统的平衡态和稳定性条件,这时无论三个波包的尺度关系如何,外源能量均能在三个波包之间传递,因此外源也可以维持三个波包的运动。进一步的结果和波包的演化过程将通过数值计算给出。