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首页> 外文期刊>Geophysical Research Letters >A DIFFICULTY WITH USING THE FROZEN FLUX HYPOTHESIS TO FIND STEADY CORE MOTIONS
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A DIFFICULTY WITH USING THE FROZEN FLUX HYPOTHESIS TO FIND STEADY CORE MOTIONS

机译:使用冻结通量假说很难找到稳定的核运动

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Many studies have used the frozen flux hypothesis to estimate core how from geomagnetic secular variation (SV). Part of the flow remains indeterminate without some additional constraint. A theorem of Voorhies and Backus states that steady flows carl be determined uniquely. Frozen flux requires the time scale of SV, tau(B), to be much shorter than the diffusion time, tau(D), and the steady motion theorem requires the time scale for change in flow, tau(V), be much longer than tau(B). Here we argue we must also have tau(V) much less than tau(D) because truly steady flow will eventually lead to a steady equilibrium magnetic field and no SV. WE illustrate tile difficulty by a numerical example with a prescribed steady flow at the top of tile core for which frozen flux inversions never yield the correct velocity. Core motions derived using the steady motions theorem may be grossly in error. [References: 14]
机译:许多研究使用冻结磁通量假说来估计岩心如何根据地磁长期变化(SV)进行估算。流程的一部分仍然不确定,没有任何其他约束。 Voorhies和Backus的一个定理指出,稳定的流量是唯一确定的。冻结通量要求SV的时间标度tau(B)要比扩散时间tau(D)短得多,稳态运动定理要求流量变化的时间标度tau(V)要长得多比tau(B)。在这里,我们认为我们还必须使tau(V)远小于tau(D),因为真正稳定的流动最终将导致产生稳定的平衡磁场而没有SV。我们通过一个数值示例来说明瓷砖难易程度,该示例在瓷砖核心顶部具有规定的稳定流,因此冻结磁通量反演永远不会产生正确的速度。使用稳定运动定理得出的核心运动可能会严重错误。 [参考:14]

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