交互式电子技术手册在舰船装备信息化保障中的应用

舰船装备的信息化保障是部队战斗力的重要因素之一。传统的装备维修保障方式已无法满足部队信息化建设的要求,通过交互式电子技术的运用,建立实时交互的舰船装备管理平台,可提高装备维修保障信息化管理的水平和效率。针对舰船装备发展趋势及维修管理的要求,采用VB软件和Access数据库编制了某型舰船装备交互式电子技术手册。通过该手册,可方便快捷地浏览、查询、添加和删除设备的三维模型、工程图、故障案例和维修标准等信息。手册的应用极大的促进了舰船装备的信息化管理水平,具有广阔的应用前景。     

GPS航海定位精度评估与分析

文章论述了GPs发展概况,包括SA取消后的美国GPS现代化对GPS应用界的影响.简述了GPS的工作原理,以及影响GPS定位精度的各种误差因素.采用OFFICE软件中的EXCEL,处理大量的实测数据,比较SA取消前后GPS定位精度,重点分析影响GPS精度的各种误差因素,对GPS民用精度进行了分析与评估.同时针对SA取消后航海应用中的定位精度,在评估GPS定位精度(2DRMS)基础上,分别采用不同版海图,实测GPS船位与在大比例尺港泊图上,通过多次陆标定位所得的平均值作为标准船位比较其偏差,分析在不同坐标系下,对船舶定位精度的影响,得出采用不同坐标系的定位误差及海图的误差.     

小型机动平台上时间配准问题分析

介绍空中移动平台传感器定位算法并建立模型,通过Monte Carlo仿真实验及内插外推法将高精度观测时间上的数据推算到低精度时间点上。该方法能同时有效地估计目标运动状态和传感器配准误差．与传统配准方法相比具有更快的收敛速度和更高的精度。     

国外激光告警技术的设备与发展

激光告警技术在现代战争中发挥着越来越重要的作用。文章介绍了激光侦察告警技术的发展历程以及装备的研制、改进情况,指出了在现代战争中发展激光侦察告警技术的优势和重要性,重点探讨了几种激光侦察告警设备性能及其特点,最后论述了激光侦察告警技术与设备的发展动向与分析。     

某雷达信号处理机的设计

信号处理是雷达系统的重要组成部分,其作用是从回波信号中提取有用信号。文章介绍了某搜索雷达信号处理机的结构及功能实现。     

排水固结地基在变荷载作用下的固结度简化分析

在瞬时加载条件下砂井地基径向固结的偏微分方程的基础上,通过编制程序,简化分析塑料板排水地基受真空及堆载的变荷载作用下的固结。工程算例分析表明,考虑加载历时的影响,地基的平均固结速度在总体上要小于瞬时加载情况下的地基固结速度;单级或分级加载情况下的地基固结度受加载时间Ti的影响,加载时间Ti越长,地基固结速度越慢。简化计算结果与考虑竖向渗流时的结果对比表明,简化方法与精确解法结果较为接近,可以满足工程精度。     

基于公共直流母线的轻型电动轮胎式集装箱门式起重机控制系统设计

对公共直流母线系统进行了分析,提出了基于公共直流母线技术的轻型电动轮胎式集装箱门式起重机（ERTG）控制系统设计方案。这套系统提高了ERTG的能量利用率,取得了良好的节能降耗和控制效果。     

航运业的四大新挑战——访丹麦海事局局长Andreas Nordseth

清瘦的丹麦海事局局长Andreas Nordseth与中国有着深厚的渊源.1979年,年轻的Andreas Nordseth作为一名船员第一次来到中国.2003年、2007年、2009年,Andreas Nordseth三度来访,每一次的中国之行,都给他留下深刻印象,中国魔术般的发展变化和独具特色的美食,让这位异国的海事官员流连忘返.     

面向深海钻井作业的波浪补偿关键技术研究

波浪补偿装置是深水钻井平台和钻井船必不可少的核心设备,文章研究了波浪补偿装置总体关键技术,根据高海情海况要求,确定钻井工况,完成总体结构研究和集成控制技术研究,形成高海情工况下研究方案,并进行位移补偿、受力补偿、减振补偿功能的仿真分析,通过试验对研究方案进行有效验证。     

Seasonal and interannual variation of physical and biological processes during 1994–2001 in the Sea of Japan/East Sea: A three-dimensional physical–biogeochemical modeling study

A Pacific basin-wide physical–biogeochemical model has been used to investigate the seasonal and interannual variation of physical and biological fields with analyses focusing on the Sea of Japan/East Sea (JES). The physical model is based on the Regional Ocean Model System (ROMS), and the biogeochemical model is based on the Carbon, Si(OH)₄, Nitrogen Ecosystem (CoSiNE) model. The coupled ROMS–CoSiNE model is forced with the daily air–sea fluxes derived from the National Centers for Environmental Prediction (NCEP) and the National Center for Atmospheric Research (NCAR) reanalysis for the period of 1994 to 2001, and the model results are used to evaluate climate impact on nutrient transport in Mixed Layer Depth (MLD) and phytoplankton spring bloom dynamics in the JES.The model reproduces several key features of sea surface temperature (SST) and surface currents, which are consistent with the previous modeling and observational results in the JES. The calculated volume transports through the three major straits show that the Korea Strait (KS) dominates the inflow to the JES with 2.46 Sv annually, and the Tsugaru Strait (TS) and the Soya Strait (SS) are major outflows with 1.85 Sv and 0.64 Sv, respectively. Domain-averaged phytoplankton biomass in the JES reaches its spring peak 1.8 mmol N m^− 3 in May and shows a relatively weak autumn increase in November. Strong summer stratification and intense consumption of nitrate by phytoplankton during the spring result in very low nitrate concentration at the upper layer, which limits phytoplankton growth in the JES during the summer. On the other hand, the higher grazer abundance likely contributes to the strong suppression of phytoplankton biomass after the spring bloom in the JES. The model results show strong interannual variability of SST, nutrients, and phytoplankton biomass with sudden changes in 1998, which correspond to large-scale changes of the Pacific Decadal Oscillation (PDO). Regional comparisons of interannual variations in springtime were made for the southern and northern JES. Variations of nutrients and phytoplankton biomass related to the PDO warm/cold phase changes were detected in both the southern and northern JES, and there were regional differences with respect to the mechanisms and timing. During the warm PDO, the nutrients integrated in the MLD increased in the south and decreased in the north in winter. Conversely, during the cold PDO, the nutrients integrated in the MLD decreased in the south and increased in the north. Wind divergence/convergence likely drives the differences in the southern and northern regions when northerly and northwesterly monsoon dominates in winter in the JES. Subjected to the nutrient change, the growth of phytoplankton biomass appears to be limited neither by nutrient nor by light consistently both in the southern and northern regions. Namely, the JES is at the transition zone of the lower trophic-level ecosystem between light-limited and nutrient-limited zones.