参考坐标系下大地水准面高度数字模型的形成方法

N. K. Shendrik
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摘要

开发了一种利用Trimble business Center软件(TBC软件)为参考坐标系生成大地水准面高度数字模型的技术。源模型可以是公开的高精度全球大地水准面高程模型EGM2008、EIGEN6C4和其他文件带有*的模型。ggf扩展与TBC软件兼容。该技术基于以ASCII格式从TBC软件导出正交高度到全球WGS-84椭球表面上用户指定区域的可能性,用于纬度和经度节点的统一网格。由此产生的数据表是计算参考坐标系的大地水准面高度的起点,根据标准,它由相应参考椭球的参数和赫尔默特参数——相对于全球坐标系的空间位置、方向和线性尺度——决定。初始数据足以计算任意参考坐标系下的大地水准面高度数字模型。所开发的技术的便利之处在于,与公认的标准值相比,它可以用于更精确地计算区域和其他领土的赫尔默特参数,因此,可以更准确地转换一般地球和参考坐标系之间的点的三维位置(这些问题将在作者随后的出版物中讨论)。该技术在几个地区得到了认可:新西伯利亚和莫斯科地区,西西伯利亚地区,白俄罗斯共和国的SK42和SK95坐标系,结果以大地水准面高程图的形式图形化呈现。
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Method of forming digital models of geoid heights for reference coordinate systems
A technique was developed for generating digital models of geoid heights for reference coordinate systems using the Trimble Bussines Center software (TBC software). The source models can be the publicly available high-precision global geoid elevation models EGM2008, EIGEN6C4 and other models whose files with the *.ggf extension are compatible with the TBC software. The technique is based on the possibility of exporting orthometric heights from the TBC software in ASCII format to a user-specified area on the surface of the global WGS-84 ellipsoid for a uniform grid of nodes in lati-tude and longitude. The resulting data table is the starting point for calculating geoid heights for reference coordinate systems, which are determined by the parameters of the corresponding reference ellipsoids and Helmert parameters - spatial position, orientation and linear scale relative to the global coordinate system, according to Standard. The initial data are sufficient to calculate the digital model of the geoid heights for an arbitrary reference coordinate system. The expediency of the developed technique lies in the possibility of its use for a much more accurate calculation of the Helmert parameters for regional and other territories compared to the accepted standard values and, accordingly, a more accurate transformation of the three-dimensional positions of points between the general earth and reference coordinate systems (these issues will be discussed in a subsequent publication by the author). Approbation of the technique was carried out for several regional territories: Novosibirsk and Moscow regions, the territory of Western Siberia, the Republic of Belarus in the SK42 and SK95 coordinate systems, and the results are presented graphically in the form of geoid height maps.
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