测绘学报 ›› 2025, Vol. 54 ›› Issue (7): 1157-1169.doi: 10.11947/j.AGCS.2025.20250141

• 大地测量学与导航 •    下一篇

地球质心、形状极与多种自转动力学参数联动的监测方法

章传银1,2,3(), 王伟1,2,3(), 蒋涛1,2,3   

  1. 1.中国测绘科学研究院空间基准全国重点实验室,北京 100036
    2.北京房山人卫激光国家野外科学观测研究站,北京 100036
    3.中国测绘科学研究院,北京 100036
  • 收稿日期:2025-04-03 修回日期:2025-07-16 出版日期:2025-08-18 发布日期:2025-08-18
  • 通讯作者: 王伟 E-mail:zhangchy@casm.ac.cn;wangwei@casm.ac.cn
  • 作者简介:章传银(1968—),男,博士,研究员,博士生导师,研究方向为大地测量与地球动力学。E-mail:zhangchy@casm.ac.cn
  • 基金资助:
    国家自然科学基金(42474012);中国测绘科学研究院基本科研业务费(AR2401)

Monitoring method of Earth's center of mass, figure pole and various rotational dynamics parameters

Chuanyin ZHANG1,2,3(), Wei WANG1,2,3(), Tao JIANG1,2,3   

  1. 1.State Key Laboratory of Spatial Datum, Chinese Academy of Surveying and Mapping, Beijing 100036, China
    2.Beijing Fangshan Satellite Laser Ranging National Observation and Research Station, Beijing 100036, China
    3.Chinese Academy of Surveying and Mapping, Beijing 100036, China
  • Received:2025-04-03 Revised:2025-07-16 Online:2025-08-18 Published:2025-08-18
  • Contact: Wei WANG E-mail:zhangchy@casm.ac.cn;wangwei@casm.ac.cn
  • About author:ZHANG Chuanyin (1968—), male, PhD, researcher, PhD supervisor, majors in geodesy and geodynamics. E-mail: zhangchy@casm.ac.cn
  • Supported by:
    The National Natural Science Foundation of China(42474012);Chinese Academy of Surveying and Mapping Basic Scientific Research Business Expense Project(AR2401)

摘要:

地球质心与形状极是描述和度量地球自转运动的大地测量基准。地球内部质量调整和物质运动无法准确测量,导致由地球物理流体数据推算的地球自转激发函数存在不确定性,制约了地球自转动力学机制的深入研究。本文通过统一大地测量和地球自转运动的地固参考系基准,解析各种大地测量要素的地球形状极变化与自转运动效应,从而发展空间几何物理大地测量协同的地球质心、形状极与多种自转动力学参数联动的监测方法,为深入研究地球自转的激发动力学机制与地球各圈层相互作用营造更有利的科学技术条件。本文主要结果包括:①推导出空间几何物理大地测量协同的地球质心与形状极定位理论,既能精密监测地球质心变化与形状极移时间序列,也能将当前地固参考系定位定向到指定时间段内的平质心和平形状极。②给出了地球卫星观测、VLBI运动学测量、地面站点径向位移和重力变化协同的地球质心、形状极与多种自转动力学参数联动的监测模型和算法,以改善地球自转动力学机理研究的约束条件。

关键词: 地固参考系, 地球质心, 地球形状极, 地球自转动力学, 大地测量协同, 地球物理激发

Abstract:

The Earth's center of mass and figure pole are geodetic datum for describing and measuring the rotation of the Earth. The inability to accurately measure mass redistribution within the Earth's interior and geomaterial motion results in more uncertainties in geophysical excitations estimated from geophysical fluid data, thereby limiting in-depth investigations into the rotational dynamics of the Earth. In this paper, various geodetic measurements and Earth rotation motion are unified in an only Earth-fixed reference system, and the effects of Earth's figure polar shift and rotation variation on various geodetic elements are investigated. And then a time-synchronized monitoring methodology for Earth's figure pole and various rotational dynamic parameters is present by multi-geodetic collaboration, which can provide more favorable scientific and technological conditions for the in-depth study of the excitation dynamics mechanism of the Earth's rotation and the interaction of the Earth's spheres. The paper presents the following main results. ① The theoretical method for positioning of Earth's center of mass and figure pole is derived by space geometric and physical geodetic collaboration, which can not only accurately measure the variation time series of Earth's center of mass and figure pole, but also position and orient the current terrestrial reference system to the mean center of mass and mean figure pole in a specified time period. ② This paper presents the monitoring algorithms of the Earth's center of mass, figure pole and various rotational dynamics parameters by collaborating with the Earth's satellite observation, VLBI kinematics measurement, and the site's radial placement and gravity variation observations, which can improve the constraints of the study on the mechanism of the Earth's rotational dynamics.

Key words: terrestrial reference system, Earth's center of mass, Earth's figure pole, Earth's rotation dynamics, multi-geodetic collaboration, geophysical excitations

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