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Inertial modes of a compressible fluid core model

机译:可压缩流体核心模型的惯性模式

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Computational methods are used to investigate the effects of fluid compressibility on the frequencies of the inertial modes of the Earth's fluid core. The 3PD (the three potential description) is applied to two models of compressible fluid spheres, for one of which the dilatation vanishes, in order to study these modes. We show that compressibility may have a significant effect on some of the modal frequencies. Using the shape of the displacement eigenfunctions of a fluid sphere we also infer which modes of a sphere may have counterparts in a spherical shell. We then give a few examples of the inertial modes of a compressible fluid shell proportional to the Earth's fluid core.
机译:使用计算方法来研究流体可压缩性对地球流体核心惯性模态频率的影响。 3PD(三个可能的描述)应用于可压缩流体球体的两个模型,其中之一消失了,以便研究这些模式。我们表明可压缩性可能会对某些模态频率产生重大影响。使用流体球体的位移本征函数的形状,我们还可以推断出球体的哪些模式在球壳中可能具有对应物。然后,我们给出一些与地球流体核成比例的可压缩流体壳的惯性模式的例子。

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