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1.
宋丹  张晓林 《海洋学报》2010,32(9):6697-6705
基于不动点理论研究了多系统兼容接收机的频点选择问题,并引入遗传算法解决了这一问题.将Banach不动点理论引入频点空间,提出并证明了频点空间中频点集的遗传进化过程反映了频点空间呈现出的一种不动点物理特性;经过频点空间算子的足够多次的反复遗传进化作用,频点空间中的任一迭代序列源频点集都将最终收敛于唯一不动点目标频点集,而该不动点目标频点集中的目标频点即为该频点选择问题的最优解.完成了遗传算法应用于频点选择问题的理论研究与实现.仿真结果表明,该算法能够有效地解决多系统兼容接收机的频点选择问题.  相似文献   

2.
史正平 《海洋学报》2010,32(9):5940-5948
研究了一个新的简易混沌振荡电路系统的稳定性和混沌特性,从理论上推导了该混沌振荡电路系统的稳定和混沌的条件,并对该系统进行了精确反馈线性化控制.最后,通过电路仿真实验和硬件实验验证了理论分析的准确性.  相似文献   

3.
刘迪  徐伟  郭培荣  倪菲 《海洋学报》2010,32(9):5934-5939
基于Lyapunov稳定性理论,设计了一个简单的标量自适应控制器分别使具有确定和不确定参数的三维(3D)二次自治混沌系统实现反同步.此外,从驱动和响应系统间的时序列动态估计出所有不确定参数. 数值仿真表明该方法的有效性和实用性.  相似文献   

4.
等效声速剖面法将实际复杂的声速剖面用一个简单的声速剖面等效替代,在声线跟踪时可以提高计算效率。但在多波束测深系统归位计算中,由于地形的起伏,对每ping各个波束使用单一的等效声速剖面会影响计算精度。通过仿真实验分析了地形起伏对等效声速剖面法计算精度的影响,提出了一种等效声速迭代算法,通过实验发现,相比于常梯度声线跟踪算法,迭代算法可达到同等精度水平,并有更高的计算效率。  相似文献   

5.
在混沌动力系统相空间重构的基础上,利用关联维数法和最大Lyapunov指数法,对平潭浪高时间序列进行混沌特性识别,并进行了预测.结果表明,浪高时间序列存在混沌现象,混沌时间序列法可应用于海浪预报的研究.  相似文献   

6.
该文采用化为积分方程组的方法 ,利用锥上不动点指数计算 ,在不要求非线性项 f (x,u)非负的情况下 ,证明 Hammerstein型非线性积分方程 φ(x) =∫Gκ(x,y) f (y,φ(y) ) dy非平凡解和多解存在性的一些新的结果。此结果可用来证明非线性常微分方程两点边值问题解的存在性。  相似文献   

7.
研究一维全局最优化问题的确定性求解方法。运用逐次建立目标函数的线性下界函数,将不含全局最优解的子区域删除,并基于非精确搜索结合下降算法而得出非精确搜索一维全局最优化方法,使计算量减少且使迭代收敛加快。迭代结束时该算法得到一维全局最优化问题的ε-全局最优解。该方法具有有限收敛性且不需精确的局部优化过程。文中的数值实例表明该算法的有效性。  相似文献   

8.
徐煜明  包伯成  徐强 《海洋学报》2010,32(9):5959-5965
基于微控制器(MCU)设计了一个通用的四维混沌系统数字硬件实验电路,由此实现了9×7网格涡卷的混沌和超混沌吸引子的生成.本文基于由Colpitts振荡器模型延伸出的四维多涡卷超混沌系统,通过引入单位锯齿波函数替换原系统中的三角波函数,构建了一个便于MCU数字硬件实现的新的网格涡卷超混沌系统,并对新系统网格涡卷吸引子的形成机理进行了分析和数值仿真.通过采用Euler算法对新系统进行离散化,在实验电路的有效动态范围内可以生成比原系统更多网格涡卷数量的吸引子.实验结果有效验证了本文基于MCU实现的网格涡卷超混沌  相似文献   

9.
矢量地图数据的加密算法   总被引:2,自引:0,他引:2  
闵连权 《海洋测绘》2005,25(2):55-57
加密技术是保障数据安全的最主要的手段,结合矢量地图数据的特点,设计了一种基于混沌序列的数据加密算法。实验证明,该算法加密效率高,保密性好。  相似文献   

10.
对我国明代华南沿海自然灾害发生次数的混沌特征分析发现 ,嵌入维数取不同值时均存在分形特征 ,且反映这种分形特征的关联维数随着嵌入维数逐渐增大而趋于一个稳定值。稳定的关联维数为 2 8,相应的饱和嵌入维数为 1 0。关联维数的稳定值为分数 (2 8)反映了控制明代华南沿海自然灾害发生次数的动力系统是一个混沌系统。构筑该系统最少需要 3个自由变量 ,最多需要 1 0个。对反映该混沌系统混沌特征强度的指标———Kolmogorov熵K值进行了计算 ,发现当嵌入维数逐渐增大到 7时K值开始稳定于 0 3 8,由此得到我国明代华南沿海自然灾害发生次数这一时间序列的可预报时间平均长度为 2 6a。  相似文献   

11.
Bin Li   《Ocean Engineering》2008,35(17-18):1842-1853
A spatial fixed σ-coordinate is used to transform the Navier–Stokes equations from the sea bed to the still water level. In the fixed σ-coordinate system only a very small number of vertical grid points are required for the numerical model. The time step for using the spatial fixed σ-coordinate is efficiently larger than that of using a time dependent σ-coordinate, as there is substantial truncation error involved in the time dependent σ-coordinate transformation. There is no need to carry out the σ-coordinate transformation at each time step, which can reduce computational times. It is important that wave breaking can be potentially modeled in the fixed σ-coordinate system, but in a time-dependent σ-coordinate system the wave breaking cannot be modeled. A projection method is used to separate advection and diffusion terms from the pressure terms in Navier–Stokes equations. The pressure variable is further separated into hydrostatic and hydrodynamic pressures so that the computer rounding errors can be largely avoided. In order to reduce computational time of solving the hydrodynamic pressure equation, at every time step the initial pressure is extrapolated in time domain using computed pressures from previous time steps, and then corrected in spatial domain using a multigrid method. For each time step, only a few of iterations (typically six iterations) are required for solving the pressure equation. The model is tested against available experimental data for regular and irregular waves and good agreement between calculation results and the measured data has been achieved.  相似文献   

12.
水下光辐射测量的阴影效应及其校正方法研究   总被引:2,自引:0,他引:2       下载免费PDF全文
用后向Monte Carlo模拟方法计算多仪器水下光学系统测量水体向上辐亮度和辐照度时由测量系统阴影导致的误差,给出了这种误差与入射太阳光相对于仪器的水平方位角之间的关系,给出了测量船对测量的影响与入射太阳光天顶角之间的关系.提出了一种辐亮度仪器自阴影误差的多光谱校正方法,模拟结果表明校正后误差小于5%.  相似文献   

13.
In this paper, a superposition of two periodic wave profiles in a finite water depth was investigated. This paper is focused on the improvement of a wave profile on the linear superposition of two waves. This improvement was realized by introducing an iterative method, which was based on a fixed point approach. Application of the fixed point approach to the wave superposition made it possible to obtain a wave profile of wave–wave interaction. The improved result of the wave profile was in good agreement with that of the nonlinear perturbation solution of the second order. It was interesting that the improved result revealed the higher-order nonlinear frequencies for two interacting Stokes waves while Dalzell's solution by a perturbation method could not predict them.  相似文献   

14.
倪飞  崔桂官 《海洋测绘》2011,31(6):28-30
为了解决空间直角坐标系间相互转换时,由于公共点的坐标精度差直接导致坐标转换精度差的问题.探讨利用抗差估计理论解决公共点坐标粗差的影响,结合具体的坐标转换算例,分别采用Tukey、IGG1及IGG3三种权函数进行迭代计算,完成坐标转换.结果表明,抗差估计原理用于空间直角坐标系间的相互转换,可以降低公共点粗差的影响,提高坐...  相似文献   

15.
A time splitting technique is common to many free surface ocean models. The different truncation errors in the equations of the internal and external modes require a numerical adjustment to make sure that algorithms correctly satisfy continuity equations and conserve tracers quantities. The princeton ocean model (POM) has applied a simple method of adjusting the vertical mean of internal velocities to external velocities at each internal time step. However, due to the Asselin time filter method adopted to prevent the numerical instability, the method of velocity adjustment used in POM can no longer guarantee the satisfaction of the continuity equation in the internal mode, though a special treatment is used to relate the surface elevation of the internal mode with that of the external mode. The error is proved to be a second-order term of the coefficient in the Asselin filter. One influence of this error in the numerical model is the failure of the kinetic boundary condition at the sea floor. By a regional experiment and a quasi-global experiment, the magni- tudes of this error are evaluated, and several sensitivity tests of this error are performed. The characteristic of this error is analyzed and two alternative algorithms are suggested to reduce the error.  相似文献   

16.
为解决单波束测深系统利用单一延迟值改正往返断面位移精度低的问题,在分析单波束测深系统误差产生原理基础上,得出往返断面位移是由系统延迟引起的固定差和换能器偏角引起的与深度相关比例误差共同作用的结果,通过建立水深与往返断面位移之间的数学模型,证实水深与断面位移具有极高相关性。利用求取单波束系统延迟及换能器偏角参数,对同一测深系统各断面形态断面进行位移改正,断面往返测数据具有良好的吻合性。证实顾及水深的单波束系统往返断面位移改正方法具有良好的系统适用性,能提高测深精度。  相似文献   

17.
In Part I of these series of papers, the complete problem formulation in a linearized form was presented. In order to provide the engineer with an in-depth knowledge about the exact solution of the problem, it is natural and essential to start with a linear solution. This will be the objective of Part II, together with an exposition to the analysis of numerical technique utilized.A truncated infinite Fourier series-type solution is adopted for the linearized boundary value problem. It is shown that such a solution is mathematically consistent and represents the phenomenon properly by satisfying all of the field equations and the imposed boundary conditions. The dependence of the Fourier coefficients on the truncation limit has been investigated. The best lower and upper “cutoff limits” for the truncation of an infinite series are determined. An error analysis of the solution technique is performed.  相似文献   

18.
Much has been written of the error in computing the baroclinic pressure gradient (BPG) with sigma coordinates in ocean or atmos- pheric numerical models. The usual way to reduce the error is to subtract area-averaged density stratification of the whole computa- tion region. But if there is great difference between the area-averaged and the local averaged density stratification, the error will be obvious. An example is given to show that the error from this method may be larger than that from no correction sometimes. The definition of local area is put forward. Then, four improved BPG difference schemes of subtracting the local averaged density strat- ification are designed to reduce the error. Two of them are for diagnostic calculation (density field is fixed), and the others are for prognostic calculation (density field is not fixed). The results show that the errors from these schemes all significantly decrease.  相似文献   

19.
G Ercilla  B Alonso  J Baraza 《Marine Geology》1994,120(3-4):249-265
The post-Calabrian sedimentary column of the northwestern Alboran Sea comprises three depositional sequences. The two older depositional sequences are defined by lowstand systems tracts (shelf-margin deltas, slope, base-of-slope, and basin deposits, and the Guadiaro channel-levee complex). In contrast, the most recent depositional sequence also includes transgressive (relict shelf facies) and high-stand (the Guadalmedina-Guadalhorce prodelta and hemipelagic facies) systems tracts. The stratigraphic architecture of these depositional sequences is controlled by the synchronism between high frequency sea-level changes, variations in sediment supply, and sedimentary processes. The configuration of the depositional sequences is variable and their distribution is complex, as a result of the relative importance played by sea-level changes and tectonism through the area.

The sequence boundaries are represented by polygenetic surfaces in the proximal margin, and by monogenetic surfaces in the distal margin and basin. Each polygenetic surface results from the interaction between the sequence boundary with the lowstand erosional truncation surface and the transgressive surface, both developed during the previous sea-level cycle. The monogenetic surfaces correspond to unconformities and their correlative conformities, formed during sea-level lowstands. This pattern of depositional sequences developed in the margin and basin of the northwestern Alboran Sea shows differences with the Exxon Sequence Stratigraphy Model as traditionally applied: sea-level change control is essentially recognized through lowstand systems tracts, and sequence boundary coincides with lowstand erosional truncation surface and transgressive surface, both developed during the previous sea-level cycle.  相似文献   


20.
驳船横荡运动下海洋立管的动力响应   总被引:1,自引:0,他引:1  
海洋浮式生产系统下立管的受力情况复杂,国内的研究大多集中于两端固支或简支的情况。本文则以水面驳船的横荡运动作为立管上端的动力边界条件,将Matteo Luca Facchinetti的尾流振子模型与考虑外流涡激振动作用下海洋立管运动微分方程相结合,得到管道与流体的耦合振动方程,用Hermit插值函数将方程进行有限元离散,并用Newmark时程分析法及迭代法求解,得到管道各点的位移时程曲线。结果表明:立管的振动频率主要由上端驳船的运动频率所确定,随着驳船运动频率的增加,立管中点的位移幅值先增加后减小;在有动边界存在的条件下,改变外流流速对立管中点的位移幅值影响不大。  相似文献   

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