Cosmic Rotational Dependency: A Hypothesized Gravitomagnetic Driver for the Secular Stability of Earth's Axial Spin
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We propose the Cosmic Rotational Dependency (CRD) hypothesis, which posits that Earth's axial rotation dynamics are significantly modulated against secular tidal dissipation through a gravitomagnetic torque arising from the Sun's \( \alpha \)--\( \Omega \) dynamo. The standard Lense--Thirring precession, driven by solar angular momentum \( J_\odot = 1.90 \times 10^{41} \) kg m\( ^2 \) s\( ^{-1} \) \citep{iorio2012}, yields a torque \( \tau_{\rm LT,std} \approx 1.97 \times 10^{14} \) N m. This is historically considered insufficient to counter the observed tidal torque \( \tau_{\rm tide} = -4.80 \times 10^{16} \) N m. We hypothesize an amplification via Einstein--Maxwell coupling in the solar interior's coherent magnetic fields (\( B_\phi \sim 10^4 \)--$10^5$ G toroidal), parameterized by \( \beta = 540^{+85}_{-70} \) (95% HDI). This mechanism yields a counter-torque capable of mitigating secular decay and inducing modulated residuals (\( \Delta {\rm LOD} \sim 0.05 \) ms over 22-yr Hale cycles). Reproducible simulations demonstrate that CRD prevents runaway rotational deceleration over Gyr timescales. Bayesian model comparison yields \( \log_{10} K = 1.85 \pm 0.12 \) favoring CRD. Falsification tests include absence of predicted LOD periodicity or \( \beta < 100 \) from LARES-2/LISA. Supported by GRMHD analogies \citep{khanna1998,tajmar2006,krolik2005} and recent solar dynamo constraints \citep{vasil2024}, CRD offers a testable resolution to planetary rotational longevity.
我们提出宇宙旋转依赖性(Cosmic Rotational Dependency,CRD)假说,该假说指出,太阳α-Ω发电机(α–Ω dynamo)产生的引力磁力矩,可显著调制地球自转动力学过程以对抗长期潮汐耗散。由太阳角动量$J_odot = 1.90 imes 10^{41} , ext{kg·m}^2· ext{s}^{-1}$[iorio, 2012]驱动的标准兰斯-蒂林进动(Lense–Thirring precession),其产生的力矩$ au_{ m LT,std} approx 1.97 imes 10^{14} , ext{N·m}$。历史上认为该力矩不足以抵消观测到的潮汐力矩$ au_{ m tide} = -4.80 imes 10^{16} , ext{N·m}$。我们提出通过太阳内部相干环向磁场(环向分量$B_phi sim 10^4$至$10^5$高斯)中的爱因斯坦-麦克斯韦耦合实现力矩放大,该过程的参数化形式为$eta = 540_{-70}^{+85}$(95%最高后验密度区间,Highest Posterior Density,HDI)。该机制产生的反力矩能够缓解地球自转的长期衰减,并诱发调制后的日长(Length of Day,LOD)残差(22年海尔周期内,日长变化$Delta ext{LOD} sim 0.05 , ext{ms}$)。可复现的模拟结果表明,CRD机制可防止地球自转在数十亿年(Gyr)的时间尺度上发生失控减速。贝叶斯模型比较得到的常用对数贝叶斯因子$log_{10} K = 1.85 pm 0.12$,支持CRD假说。证伪检验包括:若未观测到预测的日长周期性,或通过LARES-2/LISA任务得到$eta < 100$,则可否定该假说。本研究得到广义相对论磁流体动力学(General Relativistic Magnetohydrodynamics, GRMHD)类比研究[khanna, 1998; tajmar, 2006; krolik, 2005]以及近期太阳发电机约束结果[vasil, 2024]的支持,为行星自转寿命问题提供了可检验的解决方案。



