Validation of FORMOSAT-3/COSMIC radio occultation electron density profiles by incoherent scatter radar data

Low Earth Orbiting satellites carrying a dual frequency GPS receiver onboard offer a unique opportunity to remote sensing of the global ionosphere on a continuous basis. No other profiling technique unifies profiling through the entire F2-layer with global coverage. The FORMOSAT-3/COSMIC data can make a positive impact on the global ionosphere study providing essential information about the height electron density distribution and particularly over regions that are not accessible with ground-based measuring instruments such as ionosondes and GPS dual frequency receivers. Therefore, it is important to verify occultation profiles with other techniques and to obtain experience in the reliability of their derivation. In the given study we present results of comparison of the electron density profiles derived from radio occultation measurements on-board FS-3/COSMIC and from the Kharkov incoherent scatter radar sounding.     

The response of the ionosphere over Ilorin to some geomagnetic storms

The effects of some geomagnetic storms on the F2 layer peak parameters over Ilorin, Nigeria (Lat. 8:53°N, Long. 4.5°E, dip angle, −2.96°) have been investigated. Our results showed that the highest intensity of the noon bite-out occurred during the March equinox and lowest during the June Solstice on quiet days. Quiet day NmF2 disturbances which appeared as a pre-storm enhancement, but not related to the magnetic storm event that followed were observed at this station. These enhancements were attributed to the modification of the equatorial electric field as a result of injection of the Auroral electric field to the low and equatorial ionosphere. For disturbed conditions, the morphology of the NmF2 on quiet days is altered. Daytime and nighttime NmF2 and hmF2 enhancements were recorded at this station. Decreases in NmF2 were also observed during the recovery periods, most of which appeared during the post-noon period, except the storm event of May 28–29. On the average, enhancements in NmF2 (i.e. Positive phases) are the prominent features of this station. Observations from this study also indicate that Dst, Ap and Kp which have been the most widely used indices in academic research in describing the behavior of geomagnetic storms, are not sufficient for storm time analysis in the equatorial and low latitude ionosphere.     

基于CHAMP卫星观测数据对热层大气密度的经验正交分析

对2003年(太阳活动较高年)至2007年(太阳活动低年) CHAMP卫星的热层大气密度观测数据进行了经验正交函数(EOF)分析, 得到了400 km高度上白天平均大气密度ρ的太阳活动周变化与年度变化等不同变化分量. 研究结果表明, ρ受太阳活动影响较大, 其太阳周变化分量与F10.7指数变化之间的相关系数可高达94.5 %; ρ的太阳周变化分量随纬度增加而减小, 且在中高纬地区, 南半球的值明显大于北半球的值, 在低纬地区则出现基本对称的双峰分布, 即赤道质量密度异常(EMA)结构. 在ρ的年变化中, 呈现出明显的季节变化, 即夏季低冬季高; 同时ρ的年变化幅度随太阳活动增加而增强, 随纬度增加而增强. 将本文结果与经验模式NRLMSISE00在观测条件下的输出数据进行对比, 发现两者的太阳周变化与年变化分量基本一致, 但本文观测数据的太阳周成分随纬度变化略小, 年变化幅度略大, 且NRLMSISE00模式不能再现EMA结构. 研究结果对揭示热层气候学变化特征具有重要意义.      

高超声速飞行器热流密度/分层温度/碳化层研究

受试验设备能力限制,地面风洞无法完全模拟高超声速飞行器临近空间热环境。文章采用在飞行器表面开孔安装长时耐高温热流传感器直接测量热流密度的方法,国内首次获得Ma12以上高超声速飞行器表面热流密度时变数据和边界层转捩特征。实测热流值与理论预示值规律相同,两者偏差小于20%。针对树脂基材料导热微分方程中虽考虑了热解吸热项,但未考虑导热系数随温度变化情况,采用在树脂基材料导热微分方程中加入物性参数随温度变化项的方法,计算了飞行器热防护结构内部分层温度和碳化层厚度,并与实测结果进行了比较,不考虑树脂热解特性和材料物性参数随温度变化,理论值高于实测值,最大偏差275~320℃;考虑热解特性和物性参数随温度变化情况,计算值与实测值最大偏差小于70℃。     

一种提高MIMO雷达角闪烁抑制性能的方法

针对MIMO雷达体制下角闪烁引起的测角误差问题,提出了一种基于RCS自适应融合加权的抑     

航空发动机燃烧室湍流两相燃烧模型发展现状

随着计算机、计算机辅助制造等技术的发展,数值模拟逐渐成为航空发动机设计手段之一。航空发动机燃烧室内是复杂的两相湍流燃烧过程,为了准确模拟这一过程,高精度两相湍流燃烧模型组成为航空发动机燃烧室设计师 必要的工具。本文从两相湍流数值模拟角度出发,对概率密度函数输运方程模型、火焰面模型和二阶矩模型这3种常用的燃烧模型的发展现状进行简要综述。     

链路统计分析中导出参数概率计算方法研究

为了适应深空探测任务需求,有效利用测控资源,提高链路计算精度,对天地链路统计分析基本方法进行了研究,对CCSDS标准建议的3种链路参数的概率密度函数特性进行了系统分析,提出了一种当链路参数不满足李雅普诺夫（Lyapunov）条件时,利用鞍点逼近估计尾概率函数确定导出参数取值概率的方法。通过理论分析和实例计算表明,采用该方法得到的导出参数的概率分布特性与真实值基本一致,进一步完善了天地链路统计计算方法,使天地链路统计分析方法更具有普遍性。     

π-TFSK时频调制信号的功率谱分析

 高速移动数据传输时,由高速移动而产生的衰落以及多径波的干扰,传输特性及差错率特性恶化,相移时频调制正是为了对抗衰落与多径延迟而产生。建立了π-TFSK时频调制的数学模型及其复数包络模型,在π-TFSK信号的复包络自相关函数的基础上计算了π-TFSK信号的功率谱密度,并对其进行了特性分析。     

高速流动中一种关于物面密度的数值边界条件

本文结合有限元法的特点,从连续方程出发给出一种关于物面密度的数值边界条件,它可以很方便地应用于有粘或无粘高速流动的求解。