轨道参数对阿尔法磁谱仪太阳辐射热流的影响

为探明阿尔法磁谱仪（AMS）的温度变化规律,并为制定AMS的热控制方案提供指导和依据,推导了AMS重要区域（AMS前方、后方、顶部和左舷）的太阳辐射热流计算公式,分析了这些区域太阳辐射热流随轨道参数的变化,解释了AMS顶部的温度变化和太阳辐射热流变化规律在热控方案中的应用。分析表明在国际空间站（ISS）正常飞行姿态下,AMS前、后方和左舷的太阳辐射热流受太阳光与ISS轨道面的夹角（β角）、ISS与会日点的角距（θ角）和地球阴影区的影响,AMS顶部太阳辐射热流受β角和θ角的影响。得出结论：β角、θ角和地球阴影区均是影响AMS温度的主要因素,各区域的太阳辐射热流变化规律可以作为设计AMS温度控制方案的主要依据之一。     

基于LADRC的无人机高精度定高控制

针对复杂气流扰动对无人机（UAV）航迹高度控制的影响,对存在复杂气流扰动下的定高控制策略、控制结构和控制器参数优化展开研究,实现高精度高度控制。基于线性自抗扰控制（LADRC）确定总体控制架构,设计扩张状态观测器（ESO）观测估计纵向高度通道和速度通道中存在的总扰动,在控制中引入扰动补偿,减小扰动对系统输出造成的影响。对UAV在飞行过程中存在的大气紊流扰动或离散突风等风干扰分析其功率谱密度,构造考虑风扰动对高度影响、时域响应特性和稳定裕度的综合目标函数,通过粒子群优化算法得到具有高精度、高抗干扰性能的控制器参数,优化中考虑风干扰的功率谱密度分布,减小了控制器参数设计的保守性。通过与常规比例-积分-微分（PID）控制器控制效果进行对比,说明基于线性自抗扰控制器的纵向高度控制的优异性能。      

Magnetic Field Fluctuations in the Solar Wind, Foreshock and Magnetosheath： Cluster Data Analysis

46 magnetosheath crossing events from the two years (2001.2-2003.1) of Cluster magnetic field measurements are identified and used to investigate the characters of the magnetic field fluctuations in the regions of undisturbed solar wind, foreshock, magnetosheath. The preliminary results indicate the properties of the plasma turbulence in the magnetosheath are strongly controlled by IMF orientation with respect to the bow shock normal. The amplitude of the magnetic field magnitude and direction variations behind quasi-parallel bow shock are larger than those behind quasi-perpendicular bow shock. Almost purely compressional waves are found in quasi-perpendicular magnetosheath.     

Structure of the Program of Short-term Prediction of Powerful Solar Flares

Input data of the system are two-dimensional images and one-dimensional distributions of total and polarized solar emission at 5.2 cm wavelength obtained with SSRT. Together with photoheliograms, magnetograms, Hα-filtergrams and characteristics of active regions received from other sources, they form the initial database. The first stage includes superimposing the images, identifying microwave sources with active regions, assigning NOAA numbers to the sources, and determining for each active region the heliolatitude, extent, and inclination angle of the group's axis to the equator. These data are used to calculate the boundaries of longitude zones for each active region. A next stage involves determining the brightness temperatures of microwave sources less than the polarization distribution, the degree of polarization, and microwave emission flux, as well as calculating the parameters of microwave sources. Each parameter is assigned its own value of the weight factor, and the sum of values is used to draw the conclusion about the flare occurrence probability in each active region and on the Sun in general.      

结冰风洞中过冷大水滴云雾演化特性数值研究

为明晰结冰风洞中过冷大水滴（SLD）云雾演化特性,发展了基于欧拉法的SLD液滴运动、传热和传质耦合计算方法,针对3 m×2 m结冰风洞主试验段水平收缩构型,分析了SLD云雾沉降收缩特性、动量平衡特性和热平衡特性,探索了液滴变形破碎的影响,评估了构型出口处SLD液滴动量平衡和热平衡状态。研究结果表明：直径超过250 μm的SLD液滴在构型内会发生显著形变,液滴尺寸越大则变形程度越强,尤其在160 m/s工况下,当液滴直径超过750 μm后,SLD液滴甚至会发生破碎;液滴变形破碎效应会增大液滴加速度和液滴温度下降率,促使SLD液滴趋近动量平衡和热平衡状态;SLD云雾（最大液滴直径小于1 000 μm）在构型出口处会出现显著的粒径浓度分层、动量分层和热分层现象,其中直径小于100 μm的小尺寸液滴速度快、温度低且不断凝结,趋于平衡态,但直径超过500 μm的大尺寸SLD液滴速度慢、温度高且不断蒸发,则显著偏离平衡态;增大试验段气流速度尽管会减弱SLD云雾粒径浓度分层程度,但会增强动量分层和热分层程度,尤其在160 m/s工况下,SLD云雾会均匀分布在构型出口中心区域内（-0.75 m < Y < 0.75 m且-0.5 m < Z < 0.5 m）,与其平衡态间的最大速度差和温度差将分别超过18 m/s和20℃。     

利用自然能的轨迹可控临近空间浮空器初步设计

文章针对现有临近空间浮空器持久区域驻留期间面临的“超热”、“超压”和抗风机动飞行对材料和能源技术的挑战,提出一种充分利用自然界热能和准零风层风场环境的新型临近空间浮空器技术方案。文章分别介绍了新型临近空间浮空器的工作原理、系统组成、功能特点和飞行操控策略;通过浮空器热建模仿真分析和参数总体设计,研究了主气囊热控参数、浮空器白天和夜间“超热”能力,以及浮空器体积规模之间的耦合关系。结果表明,通过主气囊热控参数优化设计,可使浮空器白天“超热”值在100K以上,夜间“超热”值在20K以上,并给出了20~80K“超热”范围内的新型浮空器总体参数设计结果,这些结果满足浮空器高度调节所需浮升能力变化要求。     

基于MISG算法的风力发电机液压变桨系统故障诊断

针对受状态延时影响的风机变桨系统故障诊断,提出了一种基于多新息随机梯度(MISG)的故障诊断方法。该方法将复杂系统转化为状态空间模型,并建立系统辨识模型。将新息标量扩展成新息向量改善算法精度,利用系统发生故障引起参数改变的特征,算法对风机状态延时变桨系统完成参数估计,将系统故障诊断问题转换为系统辨识问题。仿真所得结果验证该方法可以达到诊断风机状态延时变桨系统故障的目的。     

Fundamental (f) oscillations in a magnetically coupled solar interior-atmosphere system – An analytical approach

Solar fundamental (f) acoustic mode oscillations are investigated analytically in a magnetohydrodynamic (MHD) model. The model consists of three layers in planar geometry, representing the solar interior, the magnetic atmosphere, and a transitional layer sandwiched between them. Since we focus on the fundamental mode here, we assume the plasma is incompressible. A horizontal, canopy-like, magnetic field is introduced to the atmosphere, in which degenerated slow MHD waves can exist. The global (f-mode) oscillations can couple to local atmospheric Alfvén waves, resulting, e.g., in a frequency shift of the oscillations. The dispersion relation of the global oscillation mode is derived, and is solved analytically for the thin-transitional layer approximation and for the weak-field approximation. Analytical formulae are also provided for the frequency shifts due to the presence of a thin transitional layer and a weak atmospheric magnetic field. The analytical results generally indicate that, compared to the fundamental value ($\omega =\sqrt{\mathit{gk}}$), the mode frequency is reduced by the presence of an atmosphere by a few per cent. A thin transitional layer reduces the eigen-frequencies further by about an additional hundred microhertz. Finally, a weak atmospheric magnetic field can slightly, by a few percent, increase the frequency of the eigen-mode. Stronger magnetic fields, however, can increase the f-mode frequency by even up to ten per cent, which cannot be seen in observed data. The presence of a magnetic atmosphere in the three-layer model also introduces non-permitted propagation windows in the frequency spectrum; here, f-mode oscillations cannot exist with certain values of the harmonic degree. The eigen-frequencies can be sensitive to the background physical parameters, such as an atmospheric density scale-height or the rate of the plasma density drop at the photosphere. Such information, if ever observed with high-resolution instrumentation and inverted, could help to gain further insight into solar magnetic structures by means of solar magneto-seismology, and could provide further insight into the role of magnetism in solar oscillations.     

Observation of a 27-day solar signature in noctilucent cloud altitude

Previous studies have identified solar 27-day signatures in several parameters in the Mesosphere/Lower thermosphere region, including temperature and Noctilucent cloud (NLC) occurrence frequency. In this study we report on a solar 27-day signature in NLC altitude with peak-to-peak variations of about 400?m. We use SCIAMACHY limb-scatter observations from 2002 to 2012 to detect NLCs. The superposed epoch analysis method is applied to extract solar 27-day signatures. A 27-day signature in NLC altitude can be identified in both hemispheres in the SCIAMACHY dataset, but the signature is more pronounced in the northern hemisphere. The solar signature in NLC altitude is found to be in phase with solar activity and temperature for latitudes $?70°$N. We provide a qualitative explanation for the positive correlation between solar activity and NLC altitude based on published model simulations.