地极振荡的平均频率对地极位置预测精度的影响

V. Perepelkin, D. Rumyantsev
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引用次数: 0

摘要

提出了一种确定地球极运动(地球瞬时自转轴与地球表面的交点)钱德勒振幅与年分量之比发生显著变化的时间间隔的方法。因此,在几十年的时间里,一个模型或一系列预测模型可以成功地工作,但当振幅比发生变化时,它们就变得不适用了,而应该采用与新运动更一致的其他模型。该结果用于改进地球自转模型,并选择预测磁极位置的策略,磁极的振荡由于大气和海洋环流是非线性的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The influence of the average frequency of oscillations of the Earth’s pole on the accuracy of predicting its position
A method is proposed for determining the time interval at which a significant change in the ratio of the amplitudes of the Chandler and annual components of the Earth’s pole motion (the point of intersection of the instantaneous Earth’s rotation axis with the Earth’s surface) occurs. So for several decades one model or a family of forecasting models can work successfully, but when the amplitude ratio changes, they become inapplicable and other models should be taken that are more consistent to the new movement. The result is used to refine the model of the Earth’s rotation and to select a strategy for predicting the pole position, whose oscillation due to the atmosphere and the ocean circulation is non-linear.
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