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Time variations of geopotential coefficients in the structure of the oscillatory process of the Earth's pole

机译:地球极振荡过程结构中地电势系数的时间变化

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摘要

A numerical-analytical model of the oscillatory motion of the Earth's pole is proposed with allowance for effects of time variations in geopotential coefficients. The model is a natural refinement of the earlier developed main model of pole oscillations (of Chandler and annual components) by use of celestial mechanics methods and observation data of the gravitational field of the Earth. Based on amplitude-frequency analysis and numerical simulation of the pole motion, the model allows one to offer a qualitative explanation of observed irregular phenomena in the oscillatory process and improve the forecasting accuracy for the trajectory of the pole motion. The results of numerical simulation of oscillations of the pole coordinates are presented in comparison with observation and measurement data of the International Earth Rotation Service (IERS).
机译:提出了地球极振荡运动的数值分析模型,并考虑了地势系数随时间变化的影响。该模型是利用天体力学方法和地球重力场的观测数据对极地振荡(钱德勒和年分量)早期开发的主要模型的自然改进。该模型基于振幅-频率分析和极点运动的数值模拟,可以对振荡过程中观察到的不规则现象提供定性解释,并提高极点运动轨迹的预测精度。与国际地球自转服务公司(IERS)的观测和测量数据相比较,给出了极坐标振荡的数值模拟结果。

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