The Geoid what’s it got to do with me?

R. Deakin
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引用次数: 4

Abstract

The Global Positioning System (GPS), a US Department of Defense satellite positioning system, has become a widely used measuring tool in practical surveying applications, especially in the provision of coordinate control for construction projects, small scale mapping and cadastral survey coordination. To use GPS effectively, the surveyor must be familiar with the relationships between (i) local and geocentric datums, (ii) geodetic, Australian Map Grid (AMG) and three dimensional Cartesian coordinates and (iii) heights referred to the ellipsoid, the geoid and the Australian Height Datum (AHD). These relationships, often complex, are usually expressed mathematically. The surveyor, therefore, must also be an applied mathematician - certainly by practice, if not by training. The aim of this paper is to provide an explanation of some of the mathematical theory associated with the reference surfaces and relationships mentioned above with particular attention to the geoid and GPS heighting.
大地水准面和我有什么关系?
全球定位系统(GPS)是美国国防部的卫星定位系统,已成为在实际测量应用中广泛使用的测量工具,特别是在为建设项目提供坐标控制,小比例尺测绘和地籍测量协调方面。为了有效地使用GPS,测量员必须熟悉(i)本地基准和地心基准,(ii)大地测量、澳大利亚地图网格(AMG)和三维笛卡尔坐标之间的关系,以及(iii)椭球面、大地水准面和澳大利亚高程基准(AHD)的高度。这些关系往往很复杂,通常用数学方法来表示。因此,测量员也必须是一名应用数学家——如果不是通过训练,当然是通过实践。本文的目的是提供一些与参考面和上述关系有关的数学理论的解释,特别注意大地水准面和GPS高程。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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