实时战场环境仿真系统中三维地形模型简化的研究

对实时战场环境仿真系统中三线地面模型的简化技术作了较为深入的探讨，并提出一些具有创建性的算法。     

焦作713C天气雷达异地多点实时共享方案

在省—市气象信息宽带网络通信的基础上,利用NetM eeting在ILS目录服务器的统一管理下,实现天气雷达回波图像异地多点实时共享,并采用TeamSound语音通讯系统,实现各点之间实时语音会商。     

Impacts of XBT, TAO, Altimetry and ARGO Observations on the Tropical Pacific Ocean Data Assimilation

This study aims at assessing the relative impacts of four major components of the tropical Pacific Ocean observing system on assimilation of temperature and salinity fields. Observations were collected over a period between January 2001 through June 2003 including temperature data from the expendable bathythermographs （XBT）, thermistor data from the Tropical Ocean Global Atmosphere Tropical Atmosphere-Ocean （TOGA-TAO） mooring array, sea level anomalies from the Topex/Poseidon and Jason-1 altimetry （T/P-J）, and temperature and salinity profiles from the Array for Real-time Geostrophic Oceanography （ARGO） floats. An efficient three-dimensional variational analysis-based method was introduced to assimilate the above data into the tropical-Pacific circulation model. To evaluate the impact of the individual component of the observing system, four observation system experiments were carried out. The experiment that assimilated all four components of the observing system was taken as the reference. The other three experiments were implemented by withholding one of the four components. Results show that the spatial distribution of the data influences its relative contribution. XBT observations produce the most distinguished effects on temperature analyses in the off-equatorial region due to the large amount of measurements and high quality. Similarly, the impact of TAO is dominant in the equatorial region due to the focus of the spatial distribution. The Topex/Poseidon-Jason-1 can be highly complementary where the XBT and TAO observations are sparse. The contribution of XBT or TAO on the assimilated salinity is made by the model dynamics because no salinity observations from them are assimilated. Therefore, T/P-J, as a main source for providing salinity data, has been shown to have greater impacts than either XBT or TAO on the salinity analysis. Although ARGO includes the subsurface observations, the relatively smaller number of observation makes it have the smallest contribution to the assimilation syst     

基于IGU星历的实时卫星钟差加密方法研究

主要介绍了利用IGS提供的超快速观测星历和预报星历进行5 min和30 s实时卫星钟差获取的方法,并对利用这两种星历文件获取的卫星钟差与IGS提供的最终星历做比较,最后得出结论：基于IGS的超快速观测星历采用线性模型预报实时卫星钟差的精度高于基于IGS超快速预报星历采用三次样条函数直接内插获得的实时卫星钟差的精度,可以达到3 ns,能够满足一般实时单点定位的精度要求。     

市级灾害性天气应急服务系统

灾害性天气应急服务系统是市级气象台根据实际工作需要,研制开发的灾害性天气监测、预报预警业务系统。系统实现了对灾害性天气的实时监测,预警信息编辑、制作和发布,灾情快速评估及极端灾害性天气预报应急服务等功能。介绍了系统的功能特点和业务应用情况。为市级台站做好灾害性天气监测、预报和预警应急服务等工作提供了可借鉴的思路。     

短蛸(Octopus ocellatus)酪氨酸蛋白激酶Btk基因的克隆及其mRNA在细菌刺激后的表达规律*

本研究从前期构建的短蛸cDNA文库中克隆获得了一个短蛸(Octopus ocellatus)酪氨酸蛋白激酶(OoBtk)基因的cDNA全长,其cDNA全长1191 bp,包括5’非编码区(UTR)259 bp,3’UTR 227 bp,开放阅读框(ORF)705 bp,编码234个氨基酸,预测理论等电点为8.50,分子量为27.7 kD。运用实时荧光定量PCR法分析了OoBtk在健康短蛸不同组织及鳗弧菌、藤黄微球菌刺激后短蛸血细胞中的表达规律,结果表明：OoBtk在健康短蛸肌肉、外套膜、鳃、鳃心、系统心脏、肝胰脏、肾囊、胃、性腺和血细胞等各检测组织中均有表达,其中在肝胰脏的表达量最高;短蛸经鳗弧菌和藤黄微球菌刺激后,OoBtk在血细胞中的表达量呈现出了明显的被诱导表达趋势,在鳗弧菌和藤黄微球菌刺激后6 h后表达即增强,并分别在鳗弧菌刺激后48 h和藤黄微球菌刺激后12 h达到最高。OoBtk参与短蛸对于鳗弧菌和藤黄微球菌刺激的应答过程。     

高频GNSS实时地震学与地震预警研究现状

为实现从注重灾后救助向注重灾前预防转变,如何提高地震灾害监测预警和风险防范能力成为我们关注的重点.本文给出了国际上GNSS位移记录、强震动加速度记录、测震速度记录在地震预警中的应用现状,并总结了各自的特点,归纳出围绕高频GNSS地震学在震级与破裂过程实时反演中的几个需要进一步研究的关键问题：（1）引入北斗系统,基于高频GNSS（GPS/BDS）双系统的实时位移解算方法来提高实时单站位移解算精度,使实时解算精度达到厘米级;（2）开展强震仪加速度记录基线偏移校正研究,弥补地震近场GNSS站密度不足问题;（3）强震仪加速度记录与GNSS位移记录特点不同,开展强震仪加速度数据与GNSS位移数据实时融合处理研究,快速获得包含丰富地震形变和速率的波形数据;（4）测震学方法可快速估算震级,但是在强震发生时会出现震级饱和现象,造成震级估算偏低.需要开展基于GNSS位移时间序列的多种方法相结合的实时震级估算方法研究,通过与地震学方法比较和结合,来得到精度高、计算快的震级估值算法;（5）基于高频GNSS、断层初始模型快速选取、断层尺度、参数自适应调整是快速判断断层破裂方向的基础,在断层破裂过程自适应准实时反演算法方面需要进一步加强.通过国内外研究现状调研、分析,表明基于高频GNSS地震学的震级快速确定、震源破裂过程准实时反演算法的发展将对我国地震预警系统从"二网融合"到"三网融合"提供坚实的技术支撑.     

大斜度井/水平井随钻方位电磁波测井资料实时反演方法

水平井钻进过程中,地层边界的准确预测对地质导向决策至关重要.但水平井测井环境复杂,随钻方位电磁波测井响应不直观,储层性质、地层界面等信息的精确、定量评价困难.本文提出了一种适用于大斜度井/水平井随钻方位电磁波测井资料的电阻率及地层界面信息的实时提取方法.该方法主要基于以下几个技术:(1)引入滑动开窗策略将高维随钻方位电磁波测井资料的反演问题转化为多个连续窗口的一维反演问题;(2)对反演参数进行多初值初始化,结合正则化Levenberg-Marquardt算法保证解的全局最优性;(3)充分利用随钻方位电磁波测井多种探测深度信息,采用分级反演策略提高反演速度.数值和实测资料反演结果表明:降维反演方法可实现对地层界面的实时、准确提取,且适用于多数复杂地层结构和任意井眼轨迹;利用浅探测地质信号可实现随钻方位电磁波测井资料的分级反演,最终反演速度可提升10倍以上.     

非合作目标激光测距预报的实时修正方法研究

非合作目标的激光测距预报一般是基于双行根数(TLE)外推出来的,往往有较大偏差,对激光测距的成功率有较大影响。结合空间目标的轨道理论和实测的数据分析,预报的偏差主要是预测模型外推的空间目标在运行轨道上的平近点角与实际平近点角存在偏差。根据非合作目标在望远镜跟踪视场中的脱靶量,利用相关算法可以找到一个最佳的时间根数偏差量修正空间目标的平近点角。经过修正,空间目标的视位置偏差得到改善,距离偏差能够从几百米减小到几十米,提升了预期回波到达时刻的准确度,可以给单光子探测器提供更高精度的距离门控,提高测距成功率。     

An ANN algorithm for automatic, real-time tsunami detection in deep-sea level measurements

The present paper looks at algorithms to be implemented in the software of bottom pressure recorders (BPRs) for the automatic, real-time detection of a tsunami within recorded signals. The structure of an algorithm based on the use of an artificial neural network (ANN) is presented and compared to the one developed under the Deep-ocean Assessment and Reporting of Tsunamis (DART) program run by the U.S. National Oceanic and Atmospheric Administration (NOAA). The performance and efficiency of the two algorithms are compared using both synthetic and actually measured time series. Results show that an improvement in detection performance can be obtained by using the ANN algorithm.