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首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >On the Physics of the Inner-Core Wobble; Corrections to 'Dynamics of the Inner-Core Wobble Under Mantle-Inner-Core Gravitational Interactions' by B. F. Chao
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On the Physics of the Inner-Core Wobble; Corrections to 'Dynamics of the Inner-Core Wobble Under Mantle-Inner-Core Gravitational Interactions' by B. F. Chao

机译:关于内核摆动的物理学; B. F. Chao的“披风内核重力相互作用下内核摆动的动态的校正”

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摘要

The original paper by Chao (2017, ), denoted C17, derived the period of the Earth's free inner-core wobble (ICW) with a result which was both retrograde and substantially longer than the prograde period derived by previous authors. Here we correct major errors in C17, bringing the result into better agreement with previous derivations, and clarify the role of the various torques on the Earth's inner core (IC) as presented in C17. One serious discrepancy was the magnitude of q20M, the zonal quadrupole of the mantle mass distribution, which is incorrectly evaluated in C17, with a value too large compared to those that have been previously well established for a hydrostatic Earth model. Moreover, an error in the kinematics of the ICW in C17 leads to a wrong sign for the gravitational torque exerted by the mantle on the IC. The combination of these errors led to the erroneous conclusion that the ICW is retrograde, with a much longer period (-15.6 yr) compared to previous derivations, which showed it to be prograde with a period of about +7 yr. In correcting C17, we elucidate the complete torque balance involved in the ICW.
机译:Cao(2017年)的原始纸()表示C17,源于地球的自由内核摆动(ICW)的时间,结果又逆行,并且基本上比以前作者所衍生的前期。在这里,我们在C17中纠正了重大错误,使结果与以前的派生更好地协议,并澄清了C17中提出的地球内核(IC)上的各种扭矩的作用。一种严重的差异是Q20M的幅度,在C17中在C17中不正确地评估的地幔质量分布的区间四极杆,与先前对静液压地球模型完全充分建立的那些具有过大的值。此外,C17中ICW的运动学中的误差导致错误的标志,用于IC上的地幔施加的引力扭矩。这些误差的组合导致了ICW逆行的错误结论,与之前的衍生相比,较长的时间(-15.6 YR),其显示它的促进时间为约+7年。在校正C17时,我们阐明ICW中涉及的完整扭矩平衡。

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