The interplay of fast waves and slow convection in geodynamo simulations nearing Earth’s core conditions

نویسندگان

چکیده

Ground observatory and satellite-based determinations of temporal variations in the geomagnetic field probe a decadal to annual time scale range where Earth's core slow, inertialess convective motions rapidly propagating, inertia-bearing hydromagnetic waves are interplay. Here we numerically model jointly investigate these two important features with help geodynamo simulation that (to date) is closest dynamical regime core. This also considerably enlarges scope previous asymptotic scaling analysis. Three classes hydrodynamic identified output, all propagation velocity largely exceeding advection: axisymmetric, geostrophic Alfv\'en torsional waves, non-axisymmetric, quasi-geostrophic Rossby waves. The contribution acceleration amounts an enrichment flattening its energy density spectral profile at scales, thereby providing constraint on extent $f^{-4}$ observed frequency power spectrum. flow magnetic energies carried by both linearly increase ratio diffusion scale, highlighting dominance signal stabilising control dissipation non-axisymmetric scales. Extrapolation results conditions supports detectability observations, either as axisymmetric oscillations or through jerks caused In contrast, appear be too fast carry little detectable signals limited spatio-temporal resolution.

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ژورنال

عنوان ژورنال: Geophysical Journal International

سال: 2021

ISSN: ['1365-246X', '0956-540X']

DOI: https://doi.org/10.1093/gji/ggab054