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Temperature field in the equatorial plane of the Earth's core from a high resolution numerical simulation
Version 2 2021-10-14, 08:34
Version 1 2016-06-07, 07:37
figure
posted on 2021-10-14, 08:34 authored by Nathanael SchaefferNathanael SchaefferSnapshot of temperature field in the equatorial plane of the Earth's core, from a
high resolution simulation employing spherical harmonics up to degree
893 and 1024 radial levels.
The Ekman number is E=nu/(D^2.Omega) = 10^(-7) and the magnetic Prandtl number is Pm=nu/eta=0.1
The Ekman number is E=nu/(D^2.Omega) = 10^(-7) and the magnetic Prandtl number is Pm=nu/eta=0.1
