Effects on the Ionosphere Due to Phenomena Occurring Below it

The terrestrial thermosphere and ionosphere form the most variable part of theEarth's atmosphere. Because our society depends on technological systems thatcan be affected by thermospheric and ionospheric phenomena, understanding,monitoring and ultimately forecasting the changes of the thermosphere–ionosphere system are of crucial importance to communications, navigation and the exploration of near-Earth space. The reason for the extreme variability of the thermosphere–ionosphere system isits rapid response to external forcing from various sources, i.e., thesolar ionizing flux, energetic charged particles and electric fields imposed via the interaction between the solar wind, magnetosphere and ionosphere, as well as coupling from below (meteorological influences) by the upward propagating, broad spectrum,internal atmospheric waves (planetary waves, tides, gravity waves) generated in thestratosphere and troposphere. Thunderstorms, typhoons, hurricanes, tornadoes andeven seismological events may also have observable consequences in the ionosphere.The release of trace gases due to human activity have the potential to cause changes inthe lower and the upper atmosphere.A brief overview is presented concerning the discoveries and experimentalresults that have confirmed that the ionosphere is subject to meteorologicalcontrol (especially for geomagnetic quiet conditions and for middle latitudes).D-region aeronomy, the winter anomaly of radiowave absorption, wave-liketravelling ionospheric disturbances, the non-zonality and regional peculiaritiesof lower thermospheric winds, sporadic-E occurrence and structure, spread-Fevents, the variability of ionospheric electron density profiles and Total ElectronContent, the variability of foF2, etc., should all be considered in connection withtropospheric and stratospheric processes. Ionospheric weather, as a part of spaceweather, (i.e., hour-to-hour and day-to-day variability of the ionospheric parameters)awaits explanation and prediction within the framework of the climatological, seasonal,and solar-cycle variations.     

Geodatabase数据模型在配电设备管理中的应用

首先简要介绍了Geodatabase数据模型；然后设计了Geodatabase配电网数据模型，并着重配电网中拓扑分析问题的处理；最后，利用一个简单设备介绍了Geodatabase数据模型中“复杂”节点的创建。     

Application of Fisher method to discriminating earthquakes and explosions using criterion m b/ M S

We try to give a quantitative and global discrimination function by studying m _b/M _S data using Fisher method that is a kind of pattern recognition methods. The reliability of the function is also analyzed. The results show that this criterion works well and has a global feature, which can be used as first-level filtering criterions in event identification. The quantitative and linear discrimination function makes it possible to identify events automatically and achieve the goal to react the events quickly and effectively. Contribution No.05FE3018, Institute of Geophysics, China Earthquake Administrtion.     

数字地震台网短信通系统的设计与应用

从现代移动通信短信息业务SMS出发，思考数字地震观测技术的应用新领域。介绍了DsnSMMS系统的设计方案、系统结构和主要功能。分析了OCX短信控件、系统软件、地震信息处理程序、台网实时监控程序的开发，各模块实现的功能。通过系统软件开发和短信收发设备的集成，实现了地震信息的快速群发、触发报警及台网运行状态的监控，并可以采用移动设备远程控制台网软硬件。从无锡市数字地震台网的实际应用表明，该系统智能化的交互操作与远程监控取得了良好的效果。     

基于元数据和数据集管理的空间数据共享研究

以实现地理空间数据的标准化为前提,实现数据共享及发布为目的,指出传统的基于数据集的共享模式存在着弊端,需要建立基于元数据和数据集相结合的管理机制,同时提出了元数据库设计的思想,这对于解决数据共享中的异地、异构存储是有借鉴意义的,该思想可以在数字山东的数据共享中得以实施和应用。     

永登5.8级地震序列及有关问题讨论

对永登５．８ 级地震序列及近１０ 年来永登—兰州地区的小震活动进行了研究,结果表明：永登５．８ 级地震为孤立型,震前近１０ 年震区一直有小震活动,主震是在小震活动经历了一个增多—加剧—平静的过程后才发生的。历史地震活动资料及地质构造表明,永登地区存在中强地震孕育的背景     

1997年1月21日～4月16日新疆伽师强震群综述

１９９７年１月２１日～４月１６日,新疆伽师相继发生了７次Ｍ≥６的地震,造成了破坏与伤亡。该文就伽师强震群进行了综述,包括：地震类型和地震参数;震源机制;伽师地震的临震预报;地震现场工作等。     

地震科技信息的优化管理与数据库的建立和应用

天津市地震局从贯彻执行国家地震局预测预防司的有关文件做起,结合其地震科技信息工作的特点,从优化管理入手,借助现代化的工具和手段,建立了文献管理数据库,并在实践中加以应用,以增强服务功能,更好地为防震减灾服务。     

地球空间数据元数据标准初探

论文首先概要介绍了目前有影响的几个地球空间数据元数据标准,然后从地球空间数据及数据集自身特征出发探讨了数据集元数据的内容,提出了地球空间数据集的层次结构,并给出了基本层和基础层元数据内容。