TDICCD相机在轨成像参数自主调整方法

为了改善光学遥感卫星的成像质量,提升卫星操控的灵活性,基于遥感成像理论,提出了依据太阳高度角的卫星在轨成像参数自主调整方法。文中首先讨论了影响卫星遥感成像质量的因素,分析了入瞳辐亮度随太阳高度角的变化规律及在不同侧摆角时,一个轨道周期内相机积分时间的变化范围,并据此建立了太阳高度角、侧摆角与积分级数、增益的对应关系。然后分析了太阳高度角和侧摆角的最佳分挡策略,最终得到了可用于卫星在轨成像参数自主调整的二维查找表,以实现卫星在轨成像参数自主调整。利用该方法可提升图像的辐射质量,极大减少了地面上注的数据量。     

直升机机身、平尾、垂尾的气动干扰

运用面元法模拟直升机机身流场,计算前飞状态的ROBIN(rotor body interaction)模型孤立机身顶部中线的压力系数分布,并与参考数据、CFD计算结果对比,验证了本方法的准确性.采用离散涡系模拟平尾、垂尾和短翼等升力面,以带短翼的UH-60直升机为例,研究了升力面参数变化对机身、平尾、垂尾气动干扰的影响.结果表明:改变升力面的安装角显著改变了气流对其周围的绕流情况,在参数中影响最大;平尾参数尤其是安装角会对垂尾和短翼的压力系数产生较大影响;减小垂尾展长和增大短翼安装角会提升各自的压力系数.     

舰面效应对直升机操纵的影响

舰面效应对直升机的配平操纵和姿态角有很大的影响。基于三维面元法建立了直升机舰面效应模型,可有效用于分析部分地效和倾斜甲板。最后以某型机舰配合为例,分析了舰面效应对直升机配平操纵和姿态角的影响。     

高空气球太阳能电池标定用太阳跟踪控制技术

高空气球标定的太阳能电池是可被用于地面太阳模拟器和太阳光光强检测的标准电池。首先,给出了由飞行气球搭载的高空太阳能电池标定所使用的太阳跟踪控制系统设计方法,包括基于STM32的太阳跟踪控制系统硬件设计方案、混合自动追踪控制策略、软件开发与实现方法、高空跟踪控制技术问题解决方案以及高空标定试验等。同时,解决了高空气球电池标定用太阳跟踪控制系统在极端环境下高可靠性、连续追踪和防抖动等关键技术问题。试验结果为气球飞行高度32km,平飘时间超过2h,太阳跟踪偏差小于1°。经初步分析,高空太阳跟踪控制系统标定测试结果合理可靠,工作性能稳定,为中国高空气球太阳能电池AM0标定用太阳跟踪控制系统的研究提供了新思路。     

翼尖装置优化设计研究

使用面元法气动分析软件VSAERO对机翼与翼梢小翼组合体模型进行数值模拟,并采用Steve Smith提出的诱导阻力优化方法对翼梢小翼的定位进行优化设计。结果表明,能够有效地预测出翼梢小翼的最优定位,在翼梢小翼优化设计中具有很好的适用性。     

AN IMPROVEMENT FOR LOWER－ORDER PANEL METHOD BASED ON THE DIRICHLET BOUNDARY CONDITION

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Energetic particles at high latitudes

We review work on diffusion coefficients of energetic particles with an attempt to extract implications on their behaviour at high latitudes. In the ecliptic plane results from solar energetic particle propagation between the Sun and about 5 AU can be described by an effective radial mean free path _r which is approximately constant as a function of distancer. When particle propagation in three dimensions in the heliosphere is considered it is not sufficient to consider _r only. Jovian electrons can be used as probes to determine the parameters of three-dimensional diffusion. In the polar regions diffusion is dominated by its parallel component. Some predictions how should vary with latitude are discussed. For different choices of this variation we present expectations for intensity-time profiles of solar particle events during the Ulysses polar passages.     

Type II Solar Radio Bursts: Theory and Space Weather Implications

Recent data and theory for type II solar radio bursts are reviewed, focusing on a recent analytic quantitative theory for interplanetary type II bursts. The theory addresses electron reflection and acceleration at the type II shock, formation of electron beams in the foreshock, and generation of Langmuir waves and the type II radiation there. The theory's predictions as functions of the shock and plasma parameters are summarized and discussed in terms of space weather events. The theory is consistent with available data, has explanations for radio-loud/quiet coronal mass ejections (CMEs) and why type IIs are bursty, and can account for empirical correlations between type IIs, CMEs, and interplanetary disturbances. This revised version was published online in August 2006 with corrections to the Cover Date.     

Real-Time Specifications of the Geospace Environment

We report the recent progress in our joint program of real-time mapping of ionospheric electric fields and currents and field-aligned currents through the Geospace Environment Data Analysis System (GEDAS) at the Solar-Terrestrial Environment Laboratory and similar computer systems in the world. Data from individual ground magnetometers as well as from the solar wind are collected by these systems and are used as input for the KRM and AMIE magnetogram-inversion algorithms, which calculate the two-dimensional distribution of the ionospheric parameters. One of the goals of this program is to specify the solar-terrestrial environment in terms of ionospheric processes, providing the scientific community with more than what geomagnetic activity indices and statistical models provide. This revised version was published online in August 2006 with corrections to the Cover Date.     

Modelling of the electromagnetic field in the interplanetary space and in the Earth's magnetosphere

A magnetohydrodynamic model of the solar wind flow is constructed using a kinematic approach. It is shown that a phenomenological conductivity of the solar wind plasma plays a key role in the forming of the interplanetary magnetic field (IMF) component normal to the ecliptic plane. This component is mostly important for the magnetospheric dynamics which is controlled by the solar wind electric field. A simple analytical solution for the problem of the solar wind flow past the magnetosphere is presented. In this approach the magnetopause and the Earth's bow shock are approximated by the paraboloids of revolution. Superposition of the effects of the bulk solar wind plasma motion and the magnetic field diffusion results in an incomplete screening of the IMF by the magnetopause. It is shown that the normal to the magnetopause component of the solar wind magnetic field and the tangential component of the electric field penetrated into the magnetosphere are determined by the quarter square of the magnetic Reynolds number. In final, a dynamic model of the magnetospheric magnetic field is constructed. This model can describe the magnetosphere in the course of the severe magnetic storm. The conditions under which the magnetospheric magnetic flux structure is unstable and can drive the magnetospheric substorm are discussed. The model calculations are compared with the observational data for September 24–26, 1998 magnetic storm (Dst _min=−205 nT) and substorm occurred at 02:30 UT on January 10, 1997. This revised version was published online in August 2006 with corrections to the Cover Date.