黑潮弯曲时的北太平洋冬季海温异常对大气低频振荡的影响

利用中科院大气物理研究所开放实验室ＩＡＰ－ＡＧＣＭ（二层大气环流模式），针对黑潮弯曲时的北太平洋冬季表层海温（ＳＳＴ）异常进行八个月的数值积分试验。试验结果表明：黑潮弯曲时北太平洋冬季ＳＳＴ异常对大气低频振荡的影响具有明显的３０－６０ｄ振荡的特征；在北半球的３０－６０ｄ振荡，大部分地区为向西传播，在南半球则为向东传播；其经向传播较为复杂，在１２０°Ｅ剖面上以向南传播为主；热带地区受此ＳＳＴ异常的影响以西太平洋、印度洋大气加热场的３０－６０ｄ振荡为主要标志。     

舟山市一次冬季暴雨、大风天气过程分析

应用卫星云图、常规观测资料及T213数值分析产品,分析了2004年12月3~5日发生在浙江东部地区的暴雨和舟山市沿海的大风过程。分析结果表明:这次天气过程是由台风倒槽和冷空气及深厚的高空槽共同作用引起的;台风环流引起的东南低空急流为暴雨区输送了大量的水汽和不稳定能量;冷空气的侵入加上深厚的高空槽引起的低空辐合、中高层辐散,促使了东海低压的剧烈发展,产生了猛烈的大风。     

调频输入正弦锁相环路方程周期解的存在性与稳定性

本文进一步考虑了具有正弦鉴相特性的锁相环路,我们提供了不同于文[2]的锁定参数,且求出周期解的界和渐近稳定域。     

Forces on partly buried, tandem twin cylinders in waves at low Keulegan-Carpenter numbers

This study deals with the forces on the circular cylinder, laid on, or partly buried in the bed with a parallel twin dummy cylinder nearby and without it. They were determined by measuring the pressure distribution on the cylinder in the case of wave at low KC numbers. The forces on the cylinder were calculated by the integration of the measured pressures determined by pressure transducers on the surface of the cylinder. Force coefficients were obtained for the low KC numbers (KC<5), for the burial-depth-to-the diameter ratio = 0-0.7. The distance between axis of the measurement and dummy cylinders to diameter ratio (x/D) was 2, 1.5 and 1. The dummy cylinder was replaced downstream and upstream of the measurement cylinder.     

Transformation of Wave Energy Spectrum in Shallow Water

- Combined with irregular wave-maker, the growing process of Wave Energy Spectrum in shallow water can be studied in wind wave channel on different water depth conditions, and its transformation characteristics and rules can be obtained.     

Modal Identification of Offshore Platforms Using Statistical Method Based on ERA

Identification of modal parameters of a linear structure with output-only measurements has received much attention over the past decodes. In the paper, the Natural Excitation Technique (NEXT) is used for acquisition of the impulse signals from the structural responses. Then Eigensystem Realization Algorithm (ERA) is utilized for modal identification.For disregarding the fictitious ‘computational modes’, a procedure, Statistically Averaging Modal Frequency Method (SAMFM), is developed to distinguish the true modes from noise modes, and to improve the precision of the identified modal frequencies of the structure. An offshore platform is modeled with the finite element method. The theoretical modal parameters are obtained for a comparison with the identified values. The dynamic responses of the platform under random wave loading are computed for providing the output signals used for identification with ERA. Results of simulation demonstrate that the proposed method can determine the system modal frequency with high precision.     

Time-Domain Analysis for 3-D Moored Systems

In the paper, a comprehensive numerical study on the moored system is performed in time domain. The moored system, which is composed of the floating body sub-system and the mooring line sub-system, is calculated as a whole system by coupling. A time-domain method is applied to the analysis of the mooring line sub-system, and at the same time, an indirect time-domain method translated from frequency-domain to time-domain is developed to calculate the floating body sub-system. In the end, an FPSO vessel is calculated as a numerical example by the present method. A comparison of the result of the model test and that of the numerical method indicates that the present method is exact and effective.     

近岸水域中污染羽流的运动及访问频率场模型

本文研究了由污水排海工程污水扩散器排放污水形成的污染羽流在近岸水域中的运动及访问频率场模型。在对Churchill羽流运动模拟法改进的基础上,提出了羽流分片模拟法。本方法利用质量守恒原理给出了其变化关系,并采用连续释放质点追踪法计算羽流的运动路径。考虑到非保守性物质的衰减,给出了相应的计算羽流宽度的公式。对大连市黑石礁污水排海工程方案A污染羽流(以大肠杆菌作为污染指标物)访问频率场的计算表明:访问频率场对于污水排海工程环境影响预测评价和最优排污点的选择具有十分重要的意义。     

海上结构物的Ringing现象

介绍近年来新发现的海上结构物在高海况下遇到的一种现象－－ｒｉｎｇｉｎｇ高频共振响应现象及这一现象现有的研究成果，包括该现象的发现过程、特征、产生的机理及研究方法等。提出了研究ｒｉｎｇｉｎｇ现象的一种可能的新方法。     

高频地波雷达反演海浪的海上对比验证方法研究

在介绍高频地波雷达反演海浪要素工作原理的基础上 ,利用 2 0 0 0年 10月在浙江舟山海域进行的 OSMAR2 0 0 0和 SZF1- 海上对比验证实验中所获取的资料进行系统比较分析 ,验证了OSMAR2 0 0 0探测海洋海浪要素的精度 ,并分析了 OSMAR2 0 0 0反演海浪时的误差成因