Published September 25, 2025 | Version v1
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SImulation details for Frasson et al. (2025) "Geomagnetic dipole stability and zonal flows controlled by mantle heat flux heterogeneities"

  • 1. ROR icon University of Leeds

Description

Input and output parameters of the simulations presented in Frasson et al. (2025).

Parameters:

  • nu: Viscosity
  • Omega: Rotation rate
  • D: Width of the outer core
  • eta: Magnetic diffusivity
  • g_o: Acceleration of gravity at the top of the core
  • F_i: Buoyancy flux at the bottom of the core
  • kappa: Codensity diffusivity
  • rho_0: Reference outer core density
  • U: RMS flow amplitude
  • B: RMS magnetic field amplitude

List of inputs:

  • lmax: Maximum spherical harmonic degree
  • mmax: Maximum spherical harmonic order
  • Nr_OC: Number of nodal points in the radial direction within the outer core
  • Nr_IC: Number of nodal points in the radial direction within the inner core
  • dns: True for direct numerical simulation or False for hyperdiffusive treatment
  • gprof: Radial profile of the acceleration of gravity
  • bc_icb: Flow boundary condition at the ICB
  • bc_cmb: Flow boundary condition at the CMB
  • GC: Gravitational coupling
  • CC: Inner Core conductivity
  • rratio: Aspect ratio of the outer core
  • E: Ekman number E=nu/(Omega*D^2)
  • Pm: Magnetic Prandtl number Pm=nu/eta
  • Ra: Rayleigh number Ra=g_o*F_i*D^2/(4*pi*kappa*nu^2*rho_0)
  • Pr: Prandtl number Pr=nu/kappa
  • pattern: Heterogeneous heat flux pattern at the top of the core
  • dqo/qi: Peak-to-peak amplitude of the heat flux pattern normalized by the ICB heat flux

List of outputs:

  • duration (dip. decay time): Duration of the simulation in dipole decay time unit
  • f_dip: Amplitude of the magnetic dipole at the CMB (l=1) relative to the total magnetic field at the CMB
  • E_mag: Magnetic energy
  • E_kin: Kinetic energy
  • M*_Za: Modified energy ratio (see Frasson et al. 2025, https://doi.org/10.1093/gji/ggae457)
  • ell_u: Characteristic degree of the flow
  • ell_b: Characteristic degree of the magnetic field
  • Ro_l: Local Rossby number Ro_l = U*ell_u/(pi*Omega*D)
  • Rm: Magnetic Reynolds number
  • Elsasser: Elsasser number Elsasser=B^2/(rho_0*Omega*mu_0*eta)
  • Ro_ml: Local magnetic Rossby number (see Soderlund et al. 2025, https://doi.org/10.1093/mnras/staf1081)
  • f_ohm: Fraction of ohmic dissipation

Reference:

Frasson, T., Schaeffer, N., Nataf, H. C., & Labrosse, S. (2025). Geomagnetic dipole stability and zonal flows controlled by mantle heat flux heterogeneities. Geophysical Journal International240(3), 1481-1504.

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Additional details

Related works

Is published in
Journal article: 10.1093/gji/ggae457 (DOI)

Funding

Agence Nationale de la Recherche
revEarth - Realistic modelling for Earth's magnetic field reversals ANR-19-CE31-0019

Dates

Accepted
2024-12-24