台风激发的声重力波的可探测性研究

通过对北京大学高频多普勒台站(39.4°N,116.2°E)多年的观测资料及相关台风资料的统计分析,着重研究了高频多普勒探测手段对由台风引起的扰动电离层响应的可探测性问题.通过对台风登陆前后的高频多普勒观测记录的细致分析及与宁静条件下记录的对比研究,表明高频多普勒观测手段可以很好地探测由台风激发的声重力波,尤其是对台风登陆前后所激发的扰动具有较高的可探测性.在所分析的24次台风事件中有明显扰动记录的高达22次(22/24).结合观测事实与Huang等的统计结果(2/12)进行了比较,并进行了可能的原因分析.通过数值模拟的方法对观测到的主要扰动的非线性传播过程进行了模拟再现,结果基本上与观测结果及线性传播理论一致.确认了一般情况下高可探测性这一事实,但同时也表明可探测性和台风激发源与探测位置及中尺度TIDs在电离层中的传播模式有密切关系.      

Use of global ionospheric maps for HF Doppler measurements interpretation

The HF Doppler technique, a method of measurement of Doppler frequency shift of ionospheric signal, is one of the well-known and widely used techniques of ionosphere research. It allows investigation of various disturbances in the ionosphere. There are different sources of disturbances in the ionosphere such as geomagnetic storms, solar flashes, meteorological effects and atmospheric waves. The HF Doppler technique allows us to find out the influence of earthquakes, explosions and other processes on the ionosphere, which occurs near the Earth. HF Doppler technique has high sensitivity to small frequency variations and high time resolution but interpretation of results is difficult. In this paper, we attempt to use GPS data for Doppler measurements interpretation. Modeling of Doppler frequency shift variations with use of TEC allows separation of ionosphere disturbances of medium scale.     

Observations of wave activity in the ionosphere over South Africa in geomagnetically quiet and disturbed periods

The present paper deals with observations of wave activity in the period range 1–60 min at ionospheric heights over the Western Cape, South Africa from May 2010 to July 2010. The study is based on the Doppler type sounding of the ionosphere. The Doppler frequency shift measurements are supplemented with measurements of collocated Digisonde DPS-4D at SANSA Space Sciences, Hermanus. Nine geomagnetically quiet days and nine geomagnetically active days were included in the study. Waves of periods 4–30 min were observed during the daytime independent of the level of geomagnetic activity. Amplitudes of 10–30 min waves always increased between 14:00 and 16:15 UT (16:00–18:15 LT). Secondary maxima were observed between 06:00 and 07:00 UT (08:00–09:00 LT). The maximum wave amplitudes occurred close to the time of passage of the solar terminator in the studied region which is known to act as a source of gravity waves.     

光学材料亚表面损伤深度破坏性测量技术的实验研究

基于差动原理对HF酸恒定化学蚀刻速率法进行改进,以降低环境(温度、HF酸浓度等)变化对测量结果的影响,从而提高测量效率和测量准确性。并将在新方法测量实验后的结果与理论估计值进行了比较分析。     

短波返回探测最小时延曲线的反演

提出一个利用短波扫频返回探测最小时延导出电离层结构参数的方法。这个方法不必引入辅助参数,只需给出二个频率点的最小时延数据和相应的斜率数据,即可导出电离层参数。      

1984年4月份兰州地区电离层行波扰动的观测结果及初析

１９８４年４月份兰州地区电离层行波扰动的观测结果及初析张秀菊（中国电波传播研究所,新乡,４５３００３）关键词高频返回探测,多普勒频率,电离层行波扰动１９８４年４月我们利用高频返回探测系统在新乡一西北（反射点在兰州地区）电路上多次测到电离Ｆ层的行波扰动...     

L波段有源冷噪声源研究

本文介绍了有源冷噪声源的应用背景及发展现状。根据微波场效应晶体管常温下输出稳定低噪声的特性,以Avago公司的两种典型pHEMT晶体管为核心器件进行了ADS仿真设计,研制出两款有源冷噪声源。给出了对设计的两款器件的技术指标进行验证的L波段周期定标辐射计设计框图。仿真结果表明,以pHEMT型晶体管为核心器件设计成的L波段有源冷噪声源能输出稳定低噪声。     

基于扩频体制的短波时号发播新方案及可行性分析

短波授时系统采用扩频信号将有助于提高其授时服务质量。顾及到短波信道的复杂性和系统带宽的有限性,本文提出了一种基于两个扩频信号之间的相对发播时间间隔实现短波时号发播的新方案,并对其可行性进行了分析。阐述了所提方案的基本技术思路,并通过理论分析与比较,验证了所提方案相比于常规方案能够显著降低接收机的时号检测错误概率,可更好地实现协调世界时UTC和世界时UT1两种短波时号的兼容发播,为基于扩频体制的短波时号调制技术的进一步研究提供一种有效途径。     

Method of the HF wave absorption evaluation based on GIRO network data

High frequency (HF) communication is strongly dependent on the state of the ionosphere, which specifies the mode structure of the radio wave propagating in ionosphere. Another core factor defining the strength of the HF signal at the receiving site is the ionospheric absorption. Accurate modelling the effect of absorption is an essential part of many studies of the HF propagation in the ionosphere.This paper proposes a method for estimating the absorption. The method is based on analysis of vertical sounding ionograms. The main idea of the approach is to compare the main parameters retrieved from measured and simulated ionograms. The combination of Global Ionospheric Radio Observatory (GIRO, http://giro.uml.edu) data and ionograms modelling allows for developing the empiric absorption model available at near real-time. The ionogram simulation taking into account absorption utilizes the NIM-RT (North Ionospheric Model and Ray Tracing) software. As a result, the proposed technique provides more reliable and accurate evaluation of minimum frequency at which echoes are observed in vertical incidence ionosonde soundings. The values of these frequencies should be used in the following simulation to optimize parameters in the empirical formulae for defining absorption HF wave in ionosphere.The ultimate objective of this work is the designing the method, which allows the simulating of HF radio channel accounting for regular absorption due to UV radiation of the Sun. Eventually it could be considered as some kind of the HF propagation forecasting.