细分方法是一种新的离散造型技术，细分曲面通过定义控制网格的细分规则来表示造型曲面。
Subdivision is a new method of discrete modeling. By defining the refinement rules of control meshes, subdivision surface can be considered as a method of surface modeling.
规则网格法是计算机绘制等值线的常用方法之一。
Grid contouring is one of methods often used for drawing depth contours by computers.
介绍用规则四方矩阵网格资料绘制等值线，实现天气形势检索的思路方法。
To realize searching synoptic situations, a method of drawing contours is introduced, which is based on grid data of regular square matrix.
在深入研究视频图像冗余离散变换特征的基础上，提出一种用于视频编码运动补偿技术的小波域不规则三角形网格构造方法。
This paper discusses the feature of redundant discrete wavelet transform and proposes an irregular triangular mesh design method in wavelet domain for motion compensation in wavelet video codec.
不规则分布数据的网格化处理是地球物理数据处理和解释的基础问题，是保证许多地球物理数据处理方法得以成功实施的前提。
Gridding of irregular data is a basic problem in the processing and interpretation of geophysical data, and is also an indispensable means to assure the success of geophysical data processing methods.
利用一种求偏微分方程的新方法蒙特卡罗算法通过不规则网格随机游动来求解大体积混凝土稳定温度场。
In this paper, the problem of mass concrete steady thermal field was solved by using Monte Carlo method with irregular grid random walk.
该方法在于利用直角坐标网格但通过在边界附近保留不规则控制体，使得算法是完全贴体的。
Cartesian grids were used and irregular volumes on boundary vicinity were reserved, and thus these grids were fully body fitted.
采用坐标变换方法，将物理平面中任意几何区域上的非均匀网格剖分映射到计算平面中规则区域上的均匀网格剖分。
In this paper, an one to one maping is used to transfer an arbitrary domain and a nonuniform grid on it in physical plane to a rectangular domain with a uniform grid in computational plane.
该方法通过在原始网格的基础上构造一个中间网格，再删除老顶点，可以构造一个根据曲率指导的规则网格。
This approach will generate a middle tessellation based on the initial mesh, removing the old vertices from the middle tessellation, and we can get a curvature-based regular mesh.
该方法采用数据网格树对动态数据网格进行全局控制和管理，采用挖掘作业命令的形式触发域挖掘作业，采用素数存储的方法进行了关联规则挖掘。
The method can control and manage the dynamic data grid overall situation ground, can trigger the data mining by order, can scoop out data using association rules by prime number saving.
最简单的方法是使用一个六边形网格，然后将之扰乱使它看起来不规则。
The simplest approach would be to use a hexagonal grid and perturb it a bit to make it look irregular.
建立地质构造三维可视化模型的典型方法包括三维规则网格法、TIN表面法、四面体法以及综合法。
The typical 3d visually modeling methods of geological structure include the 3d regular network model, the TIN surface model, the tetrahedron elements model and the integration model.
提出一种新的三维空间不规则网格有限差分方法，模拟具有地形构造的非均匀各向异性介质中弹性波传播过程。
This paper presents a new 3d finite-difference (FD) method using spatially irregular grids to simulate elastic wave propagation in heterogeneous anisotropic media with topographic structures.
提出一种新的三维空间不规则网格有限差分方法，模拟具有地形构造的非均匀各向异性介质中弹性波传播过程。
This paper presents a new 3d finite-difference (FD) method using spatially irregular grids to simulate elastic wave propagation in heterogeneous anisotropic media with topographic structures.
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