MAGNETOSPHERIC PHYSICS IN CHINA:2000-2002

This brief report presents the latest advances of the magnetospheric physics researches in China during the period of 2000-2002, made independently by Chinese space physicists and through international cooperation. The related areas cover almost every aspect of magnetospheric physics.     

基于对象的仿真建模系统

基于面向对象的思想，图形用户界面和仿真程序自动生成技术研制开发出一个基于对象的辅助仿真建模系统ＳｉｍＭｏｄｅｌ，介绍了ＳｉｍＭｏｄｅｌ的系统结构和模型描述框架，讨论了仿真程序生成器的运行机制，提出了有向网络图递归深广优先搜索算法。     

磁层亚暴膨胀相的近地触发模型

本文指出现有亚暴的中性线模型其源区在赤疲乏面上离地球太远；以ＧＥＯＳ－２的观测资料为依据，提出了亚暴膨胀相的一个近地触发模型－气球模不稳定性模型，该模型认为，在增长相期间到达Ｒ≈（６－１０）ＲＥ的近地等离子体片内边缘区，出现指向地球方向的离子压强梯度，越尾电流强度增大，磁力线向磁尾拉伸。当等离子体片变薄，电子沉降增强，极光带电离层电导率骤增时，气球模不稳定性在近地等离子体片内边缘区被激发，场向电流     

凹型面埋入式涡流发生器控制分离流

本文介绍了一种新型的凹型面埋入式涡流发生器的工作机理。并介绍在一个小宽高比二元单边凹壁亚声扩压壁前段出现气流分离,角落区域有倒流的情况下,采用适当几何参数的该型式涡流发生器大大减小分离区的范围,从而提高了扩压器静压恢复系数和减小总压损失系数的试验结果。     

一种小功率组合式航空发电机

先进的飞行控制系统和机载电子系统设备对轻型飞机电源系统的要求越来越高，电源系统的可靠性将直接影响到轻型飞机的安全性。本文提出了一种适用于轻型飞机的小功率组合式航空发电机方案。这种新型的“永磁─—内封闭导磁体”组合发电机既有永磁发电机的体积小、重量轻、无电刷等优点，又有内封闭导磁体发电机电压可调的优点。在发电机体积重量增加不多的情况下，免除了复杂的直流变换器，使电源系统体积最小、重量最轻，并且提高了系统的可靠性。同时采用晶体管脉宽调制激磁控制方式，使电源系统的稳压性得到提高。     

AR与ARMA有色噪声的生成方法

基于自回归与自回归滑动平均模型。讨论了两种有色噪声的软件生成方法，可使输出序列无起始瞬为现象，给定功率谱函数结构时采用递推算法。给定滤波器系数时采用步降法。分别给出了滤波器的两种设计流程。通过设置滤波器的初始状态，使得在白噪声激励下滤波器的输出序列稳定，无起始瞬变现象。     

信号源失真对波形记录仪动态有效位数评价的影响(英文)

波形记录仪和数据采集系统等设备的动态有效位数评价中,大都假定所用正弦波信号源无任何失真.当信号源具有噪声或谐波失真时,给评价结果将带来多大的影响,尚无确切的结论,这使得对有效位数评价结果无法进行量值溯源.本文从能量守衡角度,阐述了信号源噪声失真对波形记录仪动态有效位数评价结果的影响,同时给出了由输入信号源噪声和谐波失真带来影响的修正关系式,以及在给定误差限度下,信号源失真度选择原则的关系式。     

Long period magnetospheric oscillations at discrete frequencies: The results of a multi-station analysis

A multi-station analysis of geomagnetic field measurements conducted for a remarkable case event, at a European and an American array shows that, although several aspects of the geomagnetic field observations show a clear latitudinal and local time dependence, simultaneous oscillations at discrete frequencies (f ≈ 1.0, 1.3, 2.2 and 3.2 mHz) are almost ubiquitously detected, from low to high latitudes both in the light and dark sector. They are driven by fluctuations of the solar wind density and dynamic pressure at the same frequencies, via the modulation of the magnetopause current. We also report clear evidence for the occurrence of resonant coupling (at f ≈ 2.2 and 3.2 mHz) between such modes and high latitude field lines. Due to the variable length of the field line through the day, oscillation modes at the same frequencies resonate at different latitudes in the daytime and nighttime region, respectively.     

On electromagnetic phenomena in Mercury’s magnetosphere

Mercury has a small but intriguing magnetosphere. In this brief review, we discuss some similarities and differences between Mercury’s and Earth’s magnetospheres. In particular, we discuss how electric and magnetic field measurements can be used as a diagnostic tool to improve our understanding of the dynamics of Mercury’s magnetosphere. These points are of interest to the upcoming ESA-JAXA BepiColombo mission to Mercury.     

PC-index fluctuations and intermittency of the magnetospheric dynamics

One minute resolution Polar Cap (PC) index was used for the analysis of magnetospheric dynamics. The 1995–2000 time series analysis revealed that the power spectrum of the PC-index fluctuations is a power law in a wide range of frequencies. However, the obtained exponents differ for low and high frequency regions. The probability distribution functions of the PC-index fluctuations show a strong non-gaussian shape, depending on the time of increment. This indicates that the PC-index exhibits intermittency, previously detected in solar wind and auroral electrojet index fluctuations. The PC-index probability distribution functions were fitted by the functional form proposed by Castaing et al. [Velocity probability density functions of high Reynolds number turbulence. Physica D. 46, 177–200, 1990] to describe intermittency phenomena in ordinary turbulent fluid flows. The agreement between the fitting parameters obtained for the PC index and those reported before for solar wind magnetic field fluctuations is within 30%; which is noticeably less than the difference between the same parameters of solar wind and the AE-index fluctuations. This fact indicates that the PC index reflects the solar wind influence on the high-latitude magnetosphere, especially during the summer.