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A generalized theory of the figure of the Earth: on the global dynamical flattening

机译:地球图形的广义理论:关于全球动力展平

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摘要

A generalized theory of the figures of the Earth's interior to a third-order precision of ellipticity is proposed in accompanying paper in which all the odd degree and nonzero order spherical harmonic terms are included. As both the direct and indirect contributions of the asymmetric crust are included, this theory makes a significant improvement for calculating the asymmetric equilibrium figures of the real Earth comparing with the traditional theories which can only deal with the ideal symmetric Earth. The principal moments of inertia (PMOI: A, B, C) and global dynamical flattening (H) are important quantities in studying the rotating Earth. Precession and gravity observations give observation value of H (Hobs approximate to 1/305.4559) with very high precision, while its theoretical calculated value (Htheory approximate to 1/308.5) from traditional theories and a starting symmetric Earth model (like PREM model) is about 1% less than Hobs. Using the new theory in accompanying paper and replacing the homogeneous outermost crust and oceanic layers in PREM with CRUST1.0 model, we recalculate the equilibrium figures of the Earth's interior and finally get new values of PMOI and Htheory (approximate to 1/304.7167) whose consistency with Hobs are significantly improved to 0.24%. Furthermore, the asymmetric figures of some interesting boundaries, like inner core boundary, core-mantle boundary, are also given as by-products of this work as these boundaries' figures are key input for studies of their topographic effect on global rotation and geodynamics, like nutation, normal modes, especially like free core nutation.
机译:随附论文提出了地球内部数字到椭圆度三阶精度的广义理论,其中包括所有奇数阶和非零阶球谐项。由于包括了不对称地壳的直接和间接贡献,因此与仅处理理想对称地球的传统理论相比,该理论对计算真实地球的不对称平衡图作出了重大改进。在研究旋转地球时,主要惯性矩(PMOI:A,B,C)和整体动力展平(H)是重要的量。进动和重力观测可以非常精确地给出H的观测值(Hobs接近1 / 305.4559),而传统理论和初始对称地球模型(如PREM模型)的理论计算值(Hthes近似于1 / 308.5)为H。比滚刀少1%使用随附论文中的新理论,并用CRUST1.0模型替换PREM中均匀的最外层地壳和海洋层,我们重新计算了地球内部的平衡图,并最终获得了PMOI和Htheory的新值(约为1 / 304.7167),与滚刀的一致性显着提高到0.24%。此外,一些有趣的边界的非对称图形,例如内核边界,岩心-地幔边界,也作为这项工作的副产品给出,因为这些边界的图形是研究其地形对整体旋转和地球动力学的关键输入,例如章动,正常模式,尤其是自由芯章动。

著录项

  • 来源
    《Journal of Geodesy 》 |2019年第3期| 319-331| 共13页
  • 作者单位

    Chinese Acad Sci, Shanghai Astron Observ, CAS Key Lab Planetary Sci, Shanghai 200030, Peoples R China|Univ Chinese Acad Sci, Sch Astron & Space Sci, 19A Yuquan Rd, Beijing 100049, Peoples R China;

    Chinese Acad Sci, Shanghai Astron Observ, CAS Key Lab Planetary Sci, Shanghai 200030, Peoples R China|Univ Chinese Acad Sci, Sch Astron & Space Sci, 19A Yuquan Rd, Beijing 100049, Peoples R China;

    Shanghai Aerosp Control Technol Inst, Shanghai 201109, Peoples R China;

    Chinese Acad Sci, Shanghai Astron Observ, CAS Key Lab Planetary Sci, Shanghai 200030, Peoples R China|Univ Chinese Acad Sci, Sch Astron & Space Sci, 19A Yuquan Rd, Beijing 100049, Peoples R China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Figure of the Earth; Global dynamical flattening; Principal moments of inertia; Inner core boundary; Core-mantle boundary; CRUST1.0;

    机译:地球图;整体动力展平;主要惯性矩;内核边界;地幔边界;CRUST1.0;

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