船用断路器短路分断能力的换算

断路器的额定短路分断能力是由制造厂提供的，该断路器在额定频率和规定的功率因素下的分断能力值。在船舶交流电力系统中，短路时的功率因数较低，一般COSφ为0．1-0．2，为此，在设计中选用断路器时，要进行其短路分断能力换算，本文介绍船用断路器短路电流分断能力的换算。     

长江口D12灯浮附近潮流的反射迴流和突变效应

重载进出口船航行至长江口深水航道东端D12灯浮附近时,常感到有明显的横向流压。尤其是大潮汛、大风浪或鸡骨礁初涨水时,进出口船要预配10。甚至以上的风流压差,而且要加车航行,否则极易偏离航道压碰D12灯浮。此文分析长江口D12灯浮附近形成潮流的反射迴流和突变效应的原因及规律,并指出船舶在此水域航行时的注意事项,以引起航经船舶的注意。     

沥青混合料生产中冷热料数量间的协调计算

在分析沥青混合料生产过程中材料重量变化情况的基础上,建立了冷料与热料之间的换算关系,从而有效地减少溢料,为控制沥青混合料的成本提供了有效措施。     

并网逆变器的电流滞环简化控制方法

本文通过建立瞬态电流方程,分析滞环输出的周期变化规律,采用三角波形式的环宽变化规律替代正弦的环宽变化规律,在开关频率变化较小的前提下简化了相应的软件控制,并通过仿真验证了该方法的可行性。     

寒冷地区沥青混合料弯拉特性分析

文章针对寒冷地区气侯的特殊性,运用沥青混合料弯曲试验方法,分析了温度、公称最大粒径、油石比、沥青种类等因素对寒冷地区沥青混合料弯拉特性的影响及作用规律。研究结果表明：混合料油石比在6.0%～7.0%范围内取值较适宜;SBR改性沥青混合料低温性能优势显著;多年冻土地区路面设计应该重视-10℃下沥青混合料的弯曲特性,提高沥青混合料的低温性能。     

广西船舶生产企业管理探讨

文章分析了现阶段广西船舶生产企业现状及存在的主要问题,并从管理角度提出了推动船舶修造工业健康发展的对策和建议,为广西船舶生产企业提升船舶生产水平、实现跨越式发展提供思路。     

Using OMP analysis to observe temporal variability in water mass distribution

Previous optimum multiparameter analyses have investigated spatial distribution of water masses and reported successful results. This study tests the method further with application to a time series to examine temporal variability in water mass distribution. Observations collected from the Sargasso Sea are utilised, mainly to detect well-documented property changes that have occurred in Labrador Sea Water, but also possible fluctuations in water mass contributions as a whole.The results show much structure and variability in the contributions of Central Water and upper deep waters in the depth range 900–2000 m. It is proposed that the passage of warm and cold core eddies is indicated by these changes in relative contributions of water masses, although quantitative comparison of satellite altimetry data with the model results is not conclusive.Significant irregularities in the distribution of Labrador Sea Water are also revealed by the model. Through-flow of modified (since the early 1990s) Labrador Sea Water is denoted in the results by an apparent absence from mid-1995 to early 1998. This suggests a transit time of 5–6 years between the Labrador Sea and Bermuda, which is consistent with observational findings described in the literature.     

安导元整距变极法

介绍以“安导元”为基础的变极电机设计方法。用这种方法设计的变极电机线圈，无论变极前后都等效于整距线圈。首先叙述“安导元”整距变极的原理，然后给出了设计方法，并以8／2变极为例说明之。     

Quantifying uncertainty in high-resolution coupled hydrodynamic-ecosystem models

Marine ecosystem models are becoming increasingly complex and sophisticated, and are being used to estimate the effects of future changes in the earth system with a view to informing important policy decisions. Despite their potential importance, far too little attention has been, and is generally, paid to model errors and the extent to which model outputs actually relate to real-world processes. With the increasing complexity of the models themselves comes an increasing complexity among model results. If we are to develop useful modelling tools for the marine environment we need to be able to understand and quantify the uncertainties inherent in the simulations. Analysing errors within highly multivariate model outputs, and relating them to even more complex and multivariate observational data, are not trivial tasks. Here we describe the application of a series of techniques, including a 2-stage self-organising map (SOM), non-parametric multivariate analysis, and error statistics, to a complex spatio-temporal model run for the period 1988–1989 in the Southern North Sea, coinciding with the North Sea Project which collected a wealth of observational data. We use model output, large spatio-temporally resolved data sets and a combination of methodologies (SOM, MDS, uncertainty metrics) to simplify the problem and to provide tractable information on model performance. The use of a SOM as a clustering tool allows us to simplify the dimensions of the problem while the use of MDS on independent data grouped according to the SOM classification allows us to validate the SOM. The combination of classification and uncertainty metrics allows us to pinpoint the variables and associated processes which require attention in each region. We recommend the use of this combination of techniques for simplifying complex comparisons of model outputs with real data, and analysis of error distributions.     

Hydrographic cruises off northwest Africa: the Canary Current and the Cape Ghir region

We present hydrographic data for several sections located along the African coastline and off Cape Ghir, carried out at times of weak surface winds (October 1995 and September 1997). The main sections are near the continental slope, at mean distances between 100 and 150 km from the coastline. North of Cape Ghir (31°N) the geostrophic transport (referenced to 650 m) of North Atlantic Central Water through these sections is 3.7 and 2.0 Sv for 1995 and 1997, respectively. This confirms that a major fraction of the water transport by the Canary Current flows east, into the continental slope off northwest Africa, at latitudes above Cape Ghir. Most of this flow continues south past Cape Ghir, along the coast and probably through the eastern passages of the Canary Archipelago. A significant fraction, however, may escape through surface Ekman transport (0.3–0.5 Sv during the early fall season) and by offshore flow at Cape Ghir (1.1 Sv in September 1997, referenced to 650 m). Despite the weak winds the Cape Ghir filament was clearly visible, characterized by localized coastal upwelling associated to a cyclonic shallow structure and cold (and fresh) waters stretching offshore as a very shallow feature (50–100 m deep). The satellite images show that the surface temperature field is highly variable, in rapid response to the surface winds, always with a core region of relatively cold water and commonly with one or two associated eddies. Our results support the existence of two recirculation cells in the area: a horizontal one that connects the interior eastern boundary currents with the coastal region and a vertical one related to both wind-induced and filament upwelling. The data also show a salinity subsurface maximum at the root of the filament, linked to water inflow from northern latitudes, and a subsurface anticyclonic eddy over the Agadir canyon, likely related to the poleward slope undercurrent.