昆明上空电离层D区电子密度季节变化的首次观测分析

通过分析2008年8月至2009年7月昆明站(25.6°N, 103.8°E) 中频(MF)雷达观测数据, 研究了太阳活动低年电离层D区电子密度的季节变化特性,发现D区电子密度主要呈现半年变化特征, 即在春秋季电子密度较大, 而在夏冬季则较小, 这与国际参考电离层(IRI)预测的年变化趋势不一致, 但与昆明站电离层测高仪的最低回波频率f_min的观测结果相符. 同时比较了D区电子密度半年变化与纬向风半年变化的关系, 发现二者之间保持了非常一致的变化趋势并对这种一致性的内在原因进行了分析.      

火星电离层探测

火星已经成为深空探测的重要目标之一, 登陆火星并在火星生存是人类探测火星的终极目标, 因此电离层是必须了解的火星电磁环境. 火星电离层探测包括直接探测和间接探测. 直接探测精度高, 有较高的空间分辨率, 但是观测时间短, 无法提供长期稳定的探测结果. 对火星电离层的间接探测结果主要来自无线电掩星探测和顶部雷达探测. 无线电掩星探测可实现对火星电离层整个电子密度剖面的长期稳定探测, 但其空间水平分辨率较低, 且可探测的电离层太阳天顶角范围受到地球与火星轨道的限制. 顶部雷达探测对火星电离层的探测具有很高的时间分辨率和空间分辨率, 且同样可进行长期稳定探测, 为火星电离层研究提供了最新的支持. 通过对火星电离层探测的基本方法及典型观测结果的分析, 提出通过几种探测方法适当结合的方式, 同时对火星电离层进行观测, 能够大大推进对火星电离层的研究.      

橡皮液压成形工艺的可靠性稳健优化设计方法

针对当前橡皮液压成形工艺过程中材料特性、工艺参数和其他随机因素都存在的固有波动问题,面向飞机精准制造,提出了一种考虑不确定性的可靠性稳健优化设计方法.该方法基于稳健优化设计和合理的可靠性约束,对比了可靠性稳健优化解和传统优化解相关度量指标,并对2B06-O态铝合金板材橡皮成形典型的曲弯边零件进行了工艺试验验证.结果表明该方法可有效降低质量评价指标对不确定性因素的敏感度,提高了橡皮成形工艺的稳健性和可靠性.     

GPS接收机天线相位中心变化对基线解的影响

GPS接收机天线相位中心变化与卫星信号的入射方向有关，因此相位中心变化对基线解的影响还与参加解算的卫星个数及卫星的几何分布有关。在考虑卫星几何分布情况下，首先研究了相位中心变化对单个点位坐标的影响，然后推导了相位中心变化引起的基线矢量的偏差计算公式。此计算公式综合考虑了各种引起天线相位中心变化的因素，如天线的类型、天线的安置误差、卫星的几何分布、卫星个数等。最后，给出了具体算例，并给出了减弱这种影响的方法。     

高动态DS/FH混合扩频系统实现长伪码快速捕获的一种方法

针对长伪码与快速捕获的矛盾 ,设计了一种基于 FPGA技术的数字匹配滤波器 ,用于在高动态、低信噪比的 DS/ FH混合扩频系统中实现快速捕获。考虑多普勒频移的影响采用频率和码相位二维搜索。对将进入数字匹配滤波器的数据进行了降速处理 ,大大节省了硬件资源。仿真结果证明 ,采用数字匹配滤波器可在高动态环境下实现长伪码的快速捕获     

高动态环境下扩频通信系统信号快速捕获的研究

文中分析时延、多普勒频移对扩频信号相关接收的影响 ,并利用 MATLAB进行仿真 ,在此基础上给出一种高动态环境下扩频通信系统信号二维搜索方法 ,提出采用折叠匹配滤波实现伪码快速捕获。电路仿真结果表明此方法实现了长伪码 ( 1 0 2 3码长 )在高动态环境下的快速捕获 (≤ 0 .2 s)和硬件资源的合理配置     

应用端部效应改善的LS+NN模型进行日长变化预报

现有ΔLOD(Delta Length-Of-Day,日长变化)预报模式在进行周期项与残差项拟合分离时,通常没有考虑LS(Least Squares,最小二乘)拟合序列的端部效应,预报精度难以取得较大提高。针对端部效应现象,首先采用时间序列分析模型在ΔLOD序列两端进行数据延拓,构成一个新序列,然后用新序列求得LS外推模型系数,再结合LS外推模型和NN(Neural Network,神经网络)对原始ΔLOD序列进行预测。算例表明,在ΔLOD序列两端增加延拓数据,能有效改善LS拟合序列的端部效应;端部效应改善的LS+NN模型的预报精度明显优于常规LS+NN模型,精度最大提高了17.86%。该方法不仅适用于LS+NN模型,也适用于LS外推模型与其他模型的组合。     

Higher order ionospheric error correction in BDS precise orbit determination

The ionospheric error affects the accuracy of the Global Navigation Satellite Systems observation and precise orbit determination. Usually, only the first order ionospheric error is considered, which can be eliminated by the ionospheric-free linear combination observation. But the remaining higher order ionospheric error will affect the accuracy of observations and their applications. In this paper, the influence of the higher order ionospheric error have been studied by using the International Geomagnetic Reference Field 13 and the Global Ionosphere Maps model produced by the Center for Orbit Determination in Europe. Focus on ionospheric error, the experiment of paper at doy 302 in 2019, which show that the second order ionospheric error impacting BeiDou Navigation Satellite System (BDS) B1I and B3I observation is 6.3569 mm and 11.8484 mm, respectively. Whereas, the third order ionospheric error impacting BDS B1I and B3I observation is 0.1734 mm and 0.3977 mm, respectively. Due to the current measurement accuracy of BDS carrier-phase observation can reach 2 mm, the influence of high order ionospheric error on observation should be considered. For BDS precise orbit determination, the orbit overlapping results are indicated that its orbit accuracy can be improved approximately 5 mm with the higher order ionospheric error correction, which is also in agreement with the results of Satellite Laser Ranging in this work.     

An update global model of hmF2 from values estimated from ionosonde and COSMIC/FORMOSAT-3 radio occultation

In this paper, we present our recent work on developing an updated global model of the ionospheric F2 peak height hmF2 parameter by combining data from the Constellation Observing System for Meteorology, Ionosphere and Climate (COSMIC/FORMOSAT-3) radio occultation (RO) measurements and from the extended global ionosonde stations. In particular, 10 Chinese ionosonde stations’ data are newly introduced into this study. The modeling technique used is based on a two-layer empirical orthogonal function (EOF) expansion. Global distributions of hmF2 maps calculated using the newly constructed global model and the one provided by the International Reference Ionosphere model (IRI-ITU-R) are compared with the global distributions of hmF2 obtained by the COSMIC RO measurements and quantitative statistical analysis of the differences between the model results and those of the COSMIC RO measurements is made for the low (2008) and high (2012) solar activity years. The obtained average root-mean-square differences (RMSEs) for our model are 27.7 km (11.1%) and 31.0 km (9.8%), respectively for the years 2008 and 2012, whereas those for the IRI-ITU-R model are 39.9 km (16.9%) and 35.0 km (11.6%), respectively. Comparison of the results calculated both by our model and the IRI-ITU-R model with the digisonde observation is also made. The comparisons show that the newly constructed global hmF2 model can reproduce reasonably well the observations and perform better than IRI-ITU-R model.     

The occurrence of the mid-latitude ionospheric trough in GPS-TEC measurements

Simultaneous GPS observations from about 150 stations of European Permanent Network (EPN) have been used for studying dynamics of latitudinal profiles and structure of mid-latitude ionospheric trough (MIT). For the analyses, the TEC maps over Europe were created with high spatial and temporal resolution. The latitudinal profiles were produced from TEC maps with one-hour interval for geographic latitude range from 35N to 75N. The structure of latitudinal profiles relates to the occurrence of the ionospheric trough. The location of the trough depends on season, local time, and both geophysical and geomagnetic conditions. The trough structure in GPS-TEC demonstrates a smooth shape. The trough occurrence as a distinguished structure is more distinct during winter. The relation of TEC in the trough minimum to the equator and polar walls amounted to a factor of 2–4.