基于FFT的扩频信号快速捕获技术研究

在扩频通信系统中,扩频信号的快速捕获是系统功能实现的关键技术之一,同时也是一种非常重要的抗干扰手段。文章首先介绍了基于FFT的扩频信号快速捕获方法的原理,其次,针对具体实现中的一些难题,给出了采用平均相关处理的FFT快速捕获的具体实现方法,叙述了该方法的实现过程,并给出了仿真分析结果。     

基于iMPA的伪码快速捕获算法的性能分析和改进

针对迭代消息传递算法（iterative Message Passing Algorithm,iMPA）,通过证明m 序列是一种特殊的线性分组码,给出了该算法应用到伪码捕获的理论依据;分析了采用iMPA 进行伪码快速捕获的性能,包括捕获概率和算法复杂度;用马尔科夫链分析了基于iMPA的捕 获及判决流程,给出了平均捕获时间的解析表示。针对iMPA进行伪码捕获时收敛速度慢,检 测性能较低的缺点,通过增加因子图的约束,提出了冗余iMPA算法,即R\|iMPA（redundanc y iMPA）。仿真结果表明,R\|iMPA能有效的提高算法的收敛速度,检测性能平均提高约 2 dB 。     

Determination of the mean dynamic ocean topography model through combining multi-source gravity data and DTU15 MSS around China's coast

Mean dynamic ocean topography (or MDT) is closely related to ocean circulation and global climate change. It has important scientific significance and application value for the development and utilization of marine resources in China's coastal areas. Based on the terrain gravity, marine gravity, and SRTM 3?s data, an algorithm to reduce the problem of gravity data gaps between land and sea is proposed. A consistent land-sea gravity model is established based on point-mass fusion method. Then geoid model, which accuracy was estimated to be 8.5?cm through the verification of 348 GNSS/level data from the coastal provinces, of China's coastal areas was calculated through remove-restore technique. Connecting the above geoid model with DTU15 MSS model to establish a MDT model in China's coastal areas using the direct method in space domain. The effect of gravity field model, dominant factors of sea surface topography, and low pass filter are analyzed. Taking Bohai Sea and Yellow Sea as an example, and comparing MDT with the two international models CNES_2013_MDT and DTU15_MDT. The results show that the MDT has the potential to construct a vertical datum of the ocean and carry out related scientific research and application.     

北纬30°N中间层和低热层大气平均风中频雷达观测

利用武汉(30.5°N,114.4°W)中频雷达在2001年1月1日至3月18日、2002年2月5日至3月18日、2002年10月18日至12月31日期间,日本Yamagawa(31.2°N,130.6°W)中频雷达在1997年1月1日至10月17日期间的数据,分析北纬30°N地区上空60-98km高度的中间层、低热层大气平均风的变化规律,结果表明平均纬向风和经向风都具有明显的季节变化.平均纬向风在冬季基本为西风,随高度增加,西风减弱,甚至在上部会出现微弱的东风;夏季中间层表现为强烈的东风,低热层则为西风,风向转换高度在80km附近;春季和秋季为转换季节,在春季出现舌状东风结构.80km附近的平均经向风场在冬季以南风为主,在夏季则以北风为主.不同年份的平均风场存在年际变化性,但其气候变化特点非常相似.中频雷达观测结果与HWM93模式结果的气候变化特点符合很好,与其他纬度的平均纬向风气候变化特点基本类似.     

基于多层感知机的远距离水下声源定位技术研究

针对传统匹配场处理方法存在水下声源远距离定位失准以及定位时间过长的问题,提出了一种基于多层感知机的水下声源被动定位方案。利用团队自研的“浮星”浮标实测的剖面数据模拟真实海洋环境,并在水中布设垂直水听器阵,仿真大量不同位置的声源在水听器处产生的接收数据。将多通道波形数据直接作为输入对多层感知机网络进行训练,从而获取高精度的定位神经网络。仿真结果表明,与匹配场处理算法相比,设计的感知机网络可以在大范围信噪比环境中实现有效的水下声源定位,其中在30dB信噪比下定位距离和深度的平均相对误差达到了1.94%和6.84%。另外,相对于失配声速剖面,使用平均声速剖面模拟的接收数据可提高网络的定位性能。     

系统可靠性设计

预计系统的可靠性，介绍综合累计法和失效率模型，给出三种可靠性分配方法，即等分配法，ＡＧＲＥＥ法、最小努力分配法。     

弹性自由度对JJ—7飞机动态特性的影响

在小扰动假设的前提下,用正则模态法对计及弹性自由度的JJ-7飞机的纵向稳定性及操纵性进行了计算和分析,并与不计及弹性自由度飞机的动态特性进行了比较,由此讨论了弹性变形对这种类型飞机动态特性的影响。     

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。     

The contribution of local gravimetric geoid models to the calibration of satellite altimetry data and an outlook of the latest GOCE GGM performance in Gavdos

The use of geoid heights has been one of the available methodologies utilized for the independent calibration/validation of altimeters on-board satellites. This methodology has been employed for long in the Gavdos dedicated cal/val facility (Crete, Greece), where calibration results for the Jason satellites have been estimated, both for ascending and descending passes. The present work gives a detailed overview of the methodology followed in order to estimate a high-resolution and accuracy gravimetric geoid model for the wider Gavdos area, in support of the on-going calibration work. To estimate the geoid model, the well-known remove-compute-restore method is used while residual geoid heights are estimated through least-squares collocation so that associated errors are determined as well. It is found that the estimated formal geoid errors from LSC along passes 018 and 109 of Jason satellites, used for the bias estimation, range between ±0.8–1.6 cm. The so-derived geoid heights are employed in the determination of the Jason-2 altimeter bias for all available cycles (cycles 1-114, spanning the period from July 2008 to August 2011) together with the RioMed DOT model. From the results acquired the Jason-2 bias has been estimated to be +196.1 ± 3.2 mm for pass 109 and +161.9 ± 5.1 mm for pass 018. Within the same frame, the GOCE/GRACE-based geopotential model GOCO02s has been used to estimate the mean dynamic ocean topography and the steady-state circulation in the area around Gavdos. The so-derived DOT model was used to estimate the Jason-2 bias in an effort to evaluate the performance of satellite-only geoid models and investigate whether their spatial resolution and accuracy provides some improvement w.r.t. traditional local gravimetric geoids. From the results acquired with geoid heights from GOCO02s, the estimated Jason-2 bias deviates significantly from that of the local gravimetric model, which can be attributed to a possible mean offset and the low resolution of GOCE-based GGMs. On the other hand, when the newly estimated GOCE-based DOT was employed with geoid heights from the local gravimetric geoid model, the Jason-2 bias has been estimated to be +185.1 ± 3.2 mm for pass 109 and +130.2 ± 5.1 mm for pass 018.