共查询到17条相似文献，搜索用时 103 毫秒
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矢量地图数据的加密算法 总被引：2，自引：0，他引：2
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
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为提高水印的不可见性,提出1种基于水印信息压缩的图像小波域水印算法.通过细化处理和骨架缩放技术将水印图像浓缩,减少要加入的水印数据量.压缩后的水印被嵌入到图像三级小波分解后的低频逼近系统上,并通过逆过程进行水印提取,嵌入的水印具有较高的不可见性和较好稳健性.仿真实验证明算法具有很好的不可见性,经滤波、噪声、图像压缩和剪切等攻击后仍然能较好的提取水印. 相似文献
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传统的基于栅格瓦片技术生产的Web电子海图虽解决了跨浏览器显示的问题,但其显示速度、渲染效果及交互能力仍无法满足现在用户的需求。为了实现Web电子海图的大规模应用,针对栅格瓦片技术支持的下电子海图中存在的缺陷,提出基于开源地图服器Geoserver与地图可视化JS库Leaflet的矢量瓦片技术优化方案,包括海图数据预处理、矢量切片的制作、矢量瓦片数据多样式显示及矢量瓦片数据要素查询等,通过在实验室海洋信息展示平台中的验证与测试,实现了矢量电子海图数据在Web页面上的多样式灵活显示及交互功能,证实了优化方案的可行性及高效性,整体提升了Web海图服务的效率。 相似文献
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This is the first part of a publication that describes the generation of adaptive grids (this part), and simulations with vector-ocean-model (VOM) in unstructured grids resulting from the adaptation (part II). A static vertical adaptive grid in z-coordinates allows improving the approximation of topography and vertical resolution at slopes. Adaptive grids use elements from a set of grid sizes by multiplying a basic smallest cell size with powers of two, as in cell division. Grids with locally isotropic vertical resolution at surface, seabed, and slopes can be generated whereby resolution decreases towards the ocean interior. The adaptation to topography yields unstructured grids that are organised in a one-dimensional vector by column-wise storage of cells, discarding land cells. The vector storage suggested the model’s name. Grids are generated by an iterative procedure that relies on rules, i.e. criteria and directives to control the grid structure in favour of a good representation of physics and smooth numerical operations. The directives govern vertical resolution at sea surface and seabed, and at slopes. For the latter vertical resolution is extended in the horizontal. In the ocean interior horizontal distances between changes in grid size can be controlled for the sake of smooth numerics. The use of a z-grid that avoids transformation errors, the depth-independence of vertical resolution, and the lateral extension of vertical resolution at slopes towards the ocean interior are the most significant differences of adaptive grids in comparison to vertical coordinate transformations. Unstructured grids do not rely on a smoothing of topography and can be used within any of the horizontal Arakawa-grids. For the same topography directives allow creating various grids as demonstrated for a shelf-ocean topography. The number of cells per column in two unstructured grids generated for the North Atlantic may locally well exceed typical layer numbers in conventional model matrices. But the domain average is similar to layer numbers of today’s ocean models. Thus, with the same investment of cells per domain a higher resolution in slope regions can be achieved by unstructured grids as compared to conventional z-grids. 相似文献
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在进行浅海过渡带地震资料采集时,需要将电缆和检波器沉放到海底,由于洋流、潮汐等因素的影响会使检波点的实际位置与预设位置不同,从而严重影响了后续的地震资料处理工作,因此需要对检波点进行二次定位。在海底检波点二次定位中,炮点位置已知而检波点位置未知,需要从多个炮点位置正向外推波场,使波场逐步延拓到检波点,以此来获得检波点的位置。具体实现是在海底划分网格应用克希霍夫积分法外推渡场,获得网格点的能量值,能量最高的网格点便是检波点的位置。在划分网格时需要先粗分网格,求得网格点能量值,然后在能量高的网格点区域重新细分网格,通过细分网格点的能量值来确定出检波点位置。在检波点二次定位中利用的主要是直达波的波场信息,在预处理时,需要突出直达波压制干扰波。基于波动方程的检波点二次定位在模拟和实际地震资料处理中都得到了良好的效果,验证了这种方法的可行性。 相似文献
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一个水声扩频通信系统设计与实现 总被引：2，自引：0，他引：2
严重的多途衰落、多普勒频偏是水声通信中引起误码的主要原因。低功耗、远距离、高隐蔽性、低信噪比检测、高可靠性的数据传输是水声通信的一个发展方向。设计并实现了一个水声扩频通信系统,有效地解决了以上问题,并采用快速相关算法,代替传统的矢量与矩阵相乘运算,极大地减少了程序的运行量,从而实时地处理接收信号。通过湖试和海试,验证了此通信系统的优良性能。 相似文献
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基于GIS的无人机地面监控系统的设计与实现 总被引：3，自引：0，他引：3
在分析无人机领域飞行数据特征的基础上,设计实现了一套功能较为完善的无人机地面监控系统。该系统主要完成了无人机飞行状态实时显示、航线规划和航线回放等功能模块。系统借助于G IS技术,导入矢量形式的电子地图,利用丰富的地理信息来辅助实现无人机的地面监控,在V isual C 6.0开发环境下利用基于异步方式和事件驱动方式的串口通信实现了系统与地面控制站的通信,利用地图控制文件实现了地图数据的调度,利用显示缓存实现了视图实时刷新。经过实际联调,系统运行良好,实用性较好。 相似文献
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A static adaptive grid approximates the topography and defines the vertical resolution in Vector-Ocean-Model (VOM). The adaptation to topography creates unstructured grids, which are organised in a one-dimensional vector by column-wise storage of only wet cells. The model’s name reflects this data structure. The intention of VOM is better resolving flow and stratification near topographic boundaries in Z-coordinates. This is the second part of a publication that describes the generation of adaptive grids (part I), and simulations with VOM in unstructured grids (this part). Adaptive grids generated for a synthetic topography in part I include shelf, continental slope, and ocean. Three of those grids are here utilised in upwelling simulations. Under the same forcing increased vertical resolution at seabed and slopes yields a significant increase in flow energy as compared to coarser grids. Results allow explaining the surface intensification of a continental slope jet by vertical displacements of water masses in the seabed Ekman layer. Results in unstructured grids are almost identical to reference simulations in equidistant grids where the respective smallest grid size of unstructured grids was used. Negative effects of grids on predicted flow and stratification are absent also over particularly rough topography, as demonstrated by using vertical velocity as most sensitive indicator. In a further simulation an overflow governed by the advection of water mass properties is presented to demonstrate the conservation properties of the model. After 5 months of simulation the predicted domain average temperature deviated by 10−8 from the initial temperature field. Compared to equidistant grids the advection/diffusion scheme looses about one order of magnitude in accuracy when used in an unstructured grid. The results of VOM, being defined in Z-coordinates, are void of coordinate transformation errors. In an arbitrary topography unforced zero-flow remains quiescent in a stratification that only varies in the vertical. VOM due to its depth-independent vertical resolution appears particularly suitable for simulations of ocean-shelf exchange. 相似文献
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In hydrodynamic models of marine and estuarine currents the use of boundary-fitted curvilinear grids not only makes the model grids fit to the coastline and bathymetry well, but also makes the kinetic boundary conditions simple and more accurate. Because of these advantages, a three-dimensional tidal model with boundary-fitted curvilinear grids has been developed to simulate both tide and current in estuarine and shelf water. The basic idea is to use a set of coupled σ-stretched and elliptic transformations to map the physical space into a corresponding transformed space such that all boundaries are coincident with co-ordinate lines and the transformed grids are rectangular. The hydrodynamic equations in the transformed space are solved in a rectangular mesh of the transformed grid system. The application of the model in the simulation of the M2,S2 , K1and O1tidal waves in the Bohai Sea, China, shows that the numerical results are in good agreement with the observations. The method of boundary-fitted curvilinear grids is effective for improving simulation accuracy of current in the estuarine and shallow seas, especially at the coastal regions where the current was usually impractical by a uniform Cartesian grid system with the shoreline and bathymetry represented by numerous stair-steps. 相似文献