关于自由和强迫的周旋:每日的周旋

M. Ciobanu
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引用次数: 1

摘要

为了解释章动现象,欧拉选择了一个以地球为中心的坐标系来表示他的动力学方程。根据他的公式,这种章动是由某种外力引起的相对于地球中心的动量引起的。此外,波Poinsot还提出了欧拉方程的一种特殊情况,即这些外力的动量不存在。由于一个有问题的近似,Poinsot宣布在这种情况下可能会发生一个10个月的章动周期,称为“自由周期”,以区别于欧拉动力学解,称为“强迫章动”。在Poinsot之后,“自由章动”的概念也被扩展到那些只有地球物理起源,没有某些外力动量的章动现象。通常,日章动被认为是一种自由章动现象。为了寻找强迫日章动分量,使用地月质心在地球内部的日轨迹(在地心轴系中给出了该质心轨迹的简单格式)。最后,如果我们接受用地月质心来描述黄道线,那么我们也必须接受太阳和月球在恒星日间隔内对地球绕地轴自转产生的转矩。由于章动常数的值很小,需要18.6年的周期才能正确、完整地检测到强迫日章动;这种现象根据月亮升交点的经度、月亮的赤纬和太阳的黄道经度的不同,呈现出非常细微的变化。
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About the Free and Forced Nutation: The Daily Nutation
To explain the nutation phenomenon, Euler chose a geocentric frame of coordinates to present his dynamical equations. In accordance with his formulas, the nutation is caused by a momentum relative to the Earth's center, due to certain external forces. Further, Poinsot presented a special case of the Euler's equations, when any momentum of those certain external forces does not exist. Due to a problematic approximation, Poinsot announced that in this case may take place a nutation period of 10 month, named “free period”, to distinguish it from the Euler's dynamical solution, known as “forced nutation”. After Poinsot, the notion of “free nutation” was extended also to those nutation phenomena which have only a geophysical origin, without a momentum of certain external forces. Usually, the daily nutation is considered as being a free nutation phenomenon. In order to search for a forced daily nutation component, the daily trajectory of the Earth-Moon barycenter inside the Earth is used (a simple scheme of this barycenter trajectory is presented in a geocentric system of axes). Finally, if the ecliptic line is accepted to be described by the Earth-Moon barycenter, it must be accepted, too, that a torque due the Sun and the Moon acts during a sideral day interval on diurnal Earth rotation around its axis. Due to the small value of the nutation constant, a period of 18,6 years is needed to correctly and completely detect the forced daily nutation; this phenomenon permanently presents very fine variations depending on the longitude of the ascending lunar node, the Moon’s declination and the Sun’s ecliptic longitude.
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