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一个紧密结构地震台网中心核心数据处理系统

介绍一个基于UNIX类操作系统的紧密结构地震台网中心核心数据处理系统。 该系统适用于复杂结构的数字地震台网中心, 支持以比较低的成本, 可靠地完成地震台网中心的核心任务, 可以接收来自串口和网络的实时地震波形数据, 支持虚拟数字地震台网组网要求的节点数据服务功能等。 该系统的数据服务协议具有实时性高、 通讯可靠、 适应范围广等特点, 可以满足包括地震预警在内的所有实时地震数据应用的需要。 系统结构紧凑, 自动化程度高, 安全, 稳定, 系统伸缩性大, 可以满足台站数目不大于100个的数字地震台网中心的需要, 同时也可以作为大型数字地震台网中心的处理节点, 构成大型数字地震台网中心的数据处理系统。     

基于相空间重构和高斯过程回归的对流层延迟预测

天顶对流层延迟(zenith tropospheric delay,ZTD)是影响GPS定位精度的关键因素,为了提高ZTD的预测精度,提出一种基于相空间重构的高斯过程回归预测模型.针对ZTD时间序列的混沌特性,利用国际GNSS服务(International GNSS Service,IGS)站提供的ZTD数据,采用C...     

一种基于数字水印的视频多点广播立即源认证模型

基于数字水印和TESLA,提出了一种视频多点广播立即源认证模型,利用查找表的视频水印算法,将视频重要分量的消息认证码、公开密钥和立即认证散列值等嵌入到视频的非重要分量中;从而达到视频数据多点广播的立即源认证,避免了接收方数据包缓存,并给出公开延迟时间间隔d的一种计算方法。     

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Monitoring the three-dimensional ionospheric electron density distribution using GPS observations over China

In this paper, an IRI model assisted GPS-based Computerized Ionospheric Tomography (CIT) technique is developed to inverse the ionospheric electron density (IED) distribution over China. Essentially, an improved algebraic reconstruction technique (IART) is first proposed to reconstruct the ionospheric images with high resolution and high efficiency. A numerical experiment is used to validate the reliability of the method and its advantages to the classical algebraic reconstruction technique (ART). This is then used to reconstruct the IED images using the GPS data in China. The variations of the IED during magnetically quiet and disturbed days are reported and analyzed here. Reconstructed results during magnetically quiet days show some prominent ionospheric features such as the development of equatorial anomaly and the tilt of ionization crest. Meanwhile, ionospheric storm phase effects and disturbed features can also be revealed from the reconstructed IED image under storm conditions. Research shows that the positive storm phase effects usually happen in southern China, and the negative storm phase effects mainly occur in northern China. The equatorial anomaly crest moved to the north in the main phase of the storm. Ionosonde data recorded at Wuhan station provides the verification for the reliability of GPS-based CIT technique.     

小型延时多普勒雷达高度计

延时多普勒雷达高度计（Delay Doppler Radar Altimeter,DDA）是采用孔径合成技术进行高度测量的雷达高度计。与传统雷达高度计相比,DDA沿航迹方向分辨率提高了10倍,发射峰值功率降低了10dB,测高精度提高到2cm。采用DDA技术可以使仪器测量精度更高、空间分辨率更高、功耗更低,易于实现小型化。DDA代表了新一代的卫星测高技术,特别适合海洋、海岸带和极冰的测量。该文就DDA测量机理、波形仿真和精度分析进行了研究。     

重复轨道雷达干涉测量中的大气影响及其研究展望

在研究大气延迟物理机制的基础上，分析了大气效应对雷达干涉测量产生的影响，并对重复轨道雷达干涉测量中大气延迟的分析方式进行了归纳与探讨； 回顾了国内外关于InSAR大气影响的研究方法，着重对现有的大气误差改正方法进行了分类和比较，并对存在的问题进行了分析，对今后的研究方向提出了建议。     

Contribution of ionospheric irregularities to the error of dual-frequency GNSS positioning

This paper investigates the third-order residual range error in the dual-frequency correction of ionospheric effects on satellite navigation. We solve the two-point trajectory problem using the perturbation method to derive second-approximation formulas for the phase path of the wave propagating through an inhomogeneous ionosphere. It is shown that these formulas are consistent with the results derived from applying perturbation theory directly to the eikonal equation. The resulting expression for the phase path is used in calculating the residual range error of dual-frequency global positioning system (GPS) observations, in view of second- and third-order terms. The third-order correction includes not only the quadratic correction of the refractive index but also the correction for ray bending in an inhomogeneous ionosphere. Our calculations took into consideration that the ionosphere has regular large-scale irregularities, as well as smaller-scale random irregularities. Numerical examples show that geomagnetic field effects, which constitute a second-order correction, typically exceed the effects of the quadratic correction and the regular ionospheric inhomogeneity. The contribution from random irregularities can compare with or exceed that made by the second-order correction. Therefore, random ionospheric irregularities can make a significant (sometimes dominant) contribution to the residual range error.     

Medium-scale traveling ionospheric disturbances observed by GPS receiver network in Japan: a short review

Medium-scale traveling ionospheric disturbances (MSTID) are wave-like perturbations of the ionospheric plasma with wavelengths of several hundred kilometres and velocities of several hundred metres per second. MSTID is one of the most common ionospheric phenomena that generally induce the perturbations of ionospheric total electron content (TEC) by ∼10¹⁶ electron/m², which corresponds to ∼54 ns (16.2 cm) delay at GPS L1 signal. In the past decade, several new characteristics on MSTIDs have been revealed by the TEC observations using the dense GPS receiver network in Japan. In this paper, we provide a short review of these new observations and summarize the morphological characteristics of MSTIDs in Japan.