船型参数对骑浪/横甩薄弱性衡准影响研究

骑浪/横甩是IMO船舶第二代完整稳性的五种失效模式之一,是一种基于概率的稳性衡准,制定规范的目的是更有效地保障船舶在实海域中的航行安全,确保不发生稳性失效情况.本研究中,以IMO有关成员国提出的最新版骑浪/横甩薄弱性衡准草案为基础,基于自主开发的骑浪/横甩薄弱性衡准校核软件,针对围网渔船开展了样船计算和比较分析,研究IMO正在制定的骑浪/横甩薄弱性衡准方法对该类船型的适用情况,分析船型参数对骑浪/横甩薄弱性衡准的影响,为我国参与国际法规制定,提出针对骑浪/横甩薄弱性衡准的提案提供技术支撑和依据.     

采用B／S模式来实现C／S模式下物资管理系统的优化

本文通过对C／S和B／S模式物资管理系统在使用中优缺点的分析,提出了采用以C／S模式为主,B／S模式为辅的混合模式对当前单一的C／S模式物资管理系统进行改造的设想。在这种混合模式下,物资管理部门内部采用C／S模式,便于实现复杂的管理功能及可靠的安全机制：对于非物资管理部门的用户,采用B／S模式,便于统一管理与维护。最后,本文还对系统改造的开发环境和技术做了探讨。     

钦州湾围滩工程前后潮流场的数值模拟

基于双时间层的有限差分方法(ADI),建立了水深平均二维浅水潮流数学模型,采用逆风格式和追赶法求解二维浅水方程,通过建立钦州湾二维潮流数值模型重现钦州湾的潮位和潮流变化状况。模拟结果与同步进行的岸边潮位及海上潮流的观测值校验结果表明,实测潮位资料与对应时间的计算结果吻合良好,实测潮流与对应时间的计算结果十分接近。模拟计算结果真实地反映钦州湾的潮位变化和潮流运动状况。钦州湾围滩工程实施前后的潮流场数值模拟研究结果表明该工程建设不会对海域水动力学条件产生较大影响。     

C^4ISR作战系统仿真建模方法研究

对于建设C^4ISR系统来说,系统需求工程的出发点之一应该是基于对作战的描述,同时对目前作战过程进行描述的若干方法进行分析对比,结合实际情况对作战过程描述进行讨论并给出新的切入点。文章给出了一种实现C1ISR仿真系统和实装模拟系统互联的设计方案。该方案使用基于HLA的代理联邦将分布在仿真系统网络上的各个仿真节点和实装系统连接到C^4ISR仿真系统中,并通过HLA／RTI完成仿真系统与实装系统间的交互。     

应用磁天线技术解决长河二号导航系统监测问题

研制出了一款磁性天线用于解决长河二号监测系统连续监测问题并提高监测精度。磁天线相对于电天线更有利于接收长河二号信号,抑制干扰,提高信噪比,获得较高的时差测量精度,对台链各台发射信号的时间基准的调整更为准确。通过分别在导航台及监测站的试用,验证了磁性天线研制成功。     

短波并行组合扩频通信系统研究

对短波环境下并行组合扩频系统进行研究,提出一种适合短波并行组合扩频通信的MPSK软解调方法。该调制方式比并行组合扩频常采用的MASK调制方式性能更好。在扩频增益相同条件下,短波并行组合扩频通信选取结构参数r值较小（r=2）的短波并行组合扩频系统为宜。在所选择系统结构的接收端应用RAKE接收技术,仿真表明RAKE接收技术能有效抵抗多径影响,改善短波并行组合扩频系统的误码率性能。     

简化UKF算法在SINS／GPS组合导航中的应用

针对SINS／GPS组合导航系统的特点,建立了系统的非线性误差模型。根据系统状态方程为非线性而观测方程为线性的特点,将一种简化的UKF方法（Rao-Blackwellisation Additive Unscented Kalman Filter,RBAUKF）用于SINS／GPS组合导航系统中,RBAUKF采用较少的采样点数目和简化的更新算法,降低了计算复杂度。最后,在机动条件下,进行了SINS／GPS组合导航实验仿真。仿真结果表明,RBAUKF相比EKF具有更高的滤波精度,更适合在SINS／GPS组合导航系统中应用。     

基于AD2S83模拟航海罗经角位置检测研究

介绍一种模拟航海罗经的角位置检测方法,给出了实现角度测量功能的硬件电路和软件设计.着重研究了自整角机的三相信号通过隔离转换电路转换成正、余弦信号,输入到高精度AD2S83的轴角/数字转换电路转换成二进制数字信号,供给计算机系统读数显示.     

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.     

SLOPE/W软件总应力法和有效应力法的应用

按简单条分法和简化毕肖普法,通过算例阐述了SLOPE/W软件总应力法和有效应力法的计算原理和应用,指出SLOPE/W软件虽然在输入时没有区别总应力参数和有效应力参数,但结合输入时是否定义孔隙水压力,用户可以从计算方法的原理上来区别软件是按总应力法还是按有效应力法计算.