The relativistic geoid

Dennis Philipp, V. Perlick, D. Puetzfeld, E. Hackmann, C. Lämmerzahl
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引用次数: 11

Abstract

Based on the formalism of General Relativity, we analyze generalizations of concepts used in conventional geodesy. One such concept is the Earth's geoid. We present our definition of the relativistic geoid in terms of the level sets of a time-independent redshift potential. Such a potential exists for any congruence of Killing observers, i.e. for any rigidly moving object associated with a stationary spacetime in the outer region. The level surfaces of the redshift potential foliate the three dimensional space into isochronometric surfaces, which can be determined with the help of standard clocks. Two such clocks on the same surface will show zero redshift when their frequencies are compared. One of these level surfaces, singled out by a suitable convention, defines the relativistic geoid in our framework. At the same time, the redshift potential is also an acceleration potential for the congruence of observers. Hence, the isochrono-metric surfaces are orthogonal to the acceleration of freely falling objects, i.e. they are orthogonal to the local plumb line. Therefore, two independent kinds of measurements can contribute to the determination of the relativistic geoid. It can be shown that clocks, which are connected by optical fiber links, can be used to determine the redshift potential; this gives the operational foundation of our framework. Moreover, we show that our definition reduces to the well-known Newtonian and post-Newtonian notions in the respective limits. To illustrate our framework, we consider analytic examples of spacetimes, for which we calculate the level surfaces of the redshift potential and illustrate their intrinsic geometry by an embedding into flat Euclidean space. We emphasize that our definition of the geoid in terms of relativistic concepts is valid for arbitrarily strong gravitational fields. We do not use any approximation in the sense of weak fields or post-Newtonian expansion schemes. Hence, the definition can also be applied to very compact objects such as neutron stars.
相对论性大地水准面
基于广义相对论的形式主义,我们分析了传统大地测量中使用的概念的一般化。其中一个概念就是地球的大地水准面。我们用与时间无关的红移势的水平集给出了相对论性大地水准面的定义。这种势存在于任何杀戮观察者的同余,即存在于任何与外部区域的静止时空相关的刚性运动物体。红移势的水平面将三维空间切成等时面,可以借助标准时钟确定。在同一表面上的两个这样的时钟,当比较它们的频率时,红移将为零。在我们的框架中,这些平面中的一个,被一个合适的约定挑出来,定义了相对论性大地水准面。同时,红移势也是观察者同余的加速势。因此,等时曲面与自由落体的加速度正交,也就是说,它们与当地的铅垂线正交。因此,两种独立的测量方法可以帮助确定相对论性大地水准面。可以证明,通过光纤链路连接的时钟可以用来确定红移电位;这为我们的框架提供了操作基础。此外,我们还表明,我们的定义在各自的界限内简化为众所周知的牛顿和后牛顿概念。为了说明我们的框架,我们考虑了时空的解析例子,我们计算了红移势的水平表面,并通过嵌入平坦的欧几里德空间来说明它们的内在几何形状。我们强调,我们用相对论概念定义的大地水准面对于任意强的引力场是有效的。我们不使用弱场或后牛顿展开格式意义上的任何近似。因此,这个定义也可以应用于非常紧凑的物体,如中子星。
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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