海上战争中的动态海洋及动态海洋声学环境平台探讨

水声设备和其相关技术是舰船在航海中的犀利的眼睛,目前动态海洋环境已经成为水声学及其相关技术发展的瓶颈.基丁海洋地理信息、海洋气象、海洋水文及其动态物理规律的动态海洋环境系统平台,以及由此衍生的动态海洋声学环境平台,是现代海战的基本支撑环境.结合海洋学、水声学等多学科的大型综合的海洋考察实验足国外同行研究的一个前沿;共同筹建一套综合的适于现代海上战争战略战术的动态海洋环境平台,也将是我国海洋学、水声学、海军等相关领域相互协作的奋斗方向.     

高精度短时间间隔测量方法及应用

介绍了一种通过积分将短时间间隔扩展为长时间的测量方法,并对测量误差进行了分析.结果表明,应用本方法采用普通器件就可以对短时间间隔进行高精度测量,可应用于高精度小相位差测量等场合.     

1A＊冰区要求下的舵系设计

本文阐述了1A＊冰区要求下的舵系设计,主要包括舵系设计力学分析计算与舵系构件尺寸设计。     

1700TEU（GWS）船货舱通风系统设计

随着目前海运市场对运输冷藏集装箱的需求日益增多,本文结合集装箱船装载冷藏集装箱和危险品的要求,介绍1700TEU(GWS)船货舱通风系统的设计特点。     

机动车防冻冷却液的回收利用

直接排放废弃的防冻冷却液会对环境产生严重影响,本文介绍了2种防冻冷却液回收利用技术:物理蒸馏法和直接再生法,使再生液具有防腐、防锈、防垢、防沸的功能,符合防冻冷却液国家标准。     

基于Win32 API进程通信的方法研究

Microsoft Win32 API为应用程序提供了多种用于通讯和共享数据的接口,如自定义消息WM_COPYDATA、DDE(动态数据交换)、Pipe(管道)、Socket(套接字)。本文简要的介绍了这几种进程通信的实现方法及它们的优缺点。     

分光光度计测量结果的不确定度评定

测量不确定度是对测量结果而言,表达这个结果分散性程度的参数,是计量学中的一个重要内容。本文对分光光度计校准过程的透射比示值误差测量结果的不确定度和波长示值误差测量结果的不确定度进行了评定,给出了评定方法、步骤及结果,并对测量不确定度进行了讨论。     

Spatial variability of the barotropic M2 constituent tidal current over the Rías Baixas Galician shelf (NW Spain)

Using current meters and systematically repeated vessel mounted ADCP data legs, we describe the role of the semidiurnal and diurnal constituents in the tidal currents and investigate the mesoscale variability of the M₂ tidal currents field along three cross-shelf legs over the Galician shelf. We found that the estimated values of the semi-major axes of the main semidiurnal tidal constituents are closely related to those obtained in previous research and that the tidal currents are predominantly semidiurnal. Amplitudes of the M₂ and S₂ semi-major axes constituents are comparable, and important fortnightly variability should thus be expected in the amplitude of the semidiurnal tidal currents. Vertical profiles of the semi-major axes of the main tidal constituents reveal that, in the absence of stratification, and far from the bottom frictional effects, the tidal currents are mostly barotropic. Over the slope, the tidal ellipses tilt from a north–south orientation toward the northeast–southwest direction and, as we go further into the shelf, their amplitude is increased, a feature that is reasonably explained by the transition from the dynamics of a Poincaré wave offshore to the dynamics of a northward alongshore propagating Kelvin wave over the shelf. The Ría de Vigo exerts a notable influence over the tidal currents, acting as an extension of the shelf and introducing a meridional variation in the orientation of the ellipses from the alongshore direction in the southern straight coast toward the northeast–southwest direction at the latitude of the Rías. Finally, the spatial fitting methods we tried have proved to be successful in VMADCP data detiding in this region.     

Hydrographic conditions affecting two fishing grounds of Mallorca island (Western Mediterranean): during the IDEA Project (2003–2004)

This paper describes the hydrographic conditions observed during six surveys carried out during 2003 and 2004, in the framework of the “IDEA Project” (acronym for “Influence of oceanographic structure and dynamics on demersal populations in waters of the Balearic Islands”). The surveys were developed on the shelf and slope of Mallorca Island, in particular in two fishing grounds at the north and south of the Mallorca channel. Periodic movements of the fishing fleet between these two areas have been regularly reported, suggesting a seasonal variability of the resources which could be in turn associated with the hydrodynamic variability. With this motivation, water masses affecting these grounds have been identified and their seasonal variability has been studied. Different oceanographic and environmental conditions have been found between the two fishing grounds. These differences are related to the presence of mesoscale structures, associated with the Western Mediterranean Intermediate Water (WIW) at the north of the Ibiza channel and big gyres detached from the Algerian Current. The former has been shown to have influence on the regional oceanic circulation and the latter could affect the progress of fresh Atlantic Water (AW) towards the channels and make possible the presence of high salinity values at intermediate waters at the south of Mallorca Island. Historical data from other oceanographic cruises carried out in the region are finally used to discuss the interannual variability of these mesoscale structures.