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Zonal flow driven by deep convection in the major planets
Author(s) -
Christensen Ulrich R.
Publication year - 2001
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2000gl012643
Subject(s) - ekman number , planet , convection , zonal flow (plasma) , saturn , radius , rayleigh number , jupiter (rocket family) , physics , outer planets , geophysics , uranus , mechanics , spherical shell , geology , flow (mathematics) , shell (structure) , natural convection , astronomy , materials science , spacecraft , plasma , computer security , quantum mechanics , computer science , composite material , tokamak
The cause of the fast zonal winds on the large gas planets is disputed. To investigate their possible origin by convection in the planets' molecular hydrogen layer, I study simple numerical models of thermal convection in a rotating sphere at low Ekman numbers for Rayleigh numbers up to 100 times critical. With stress‐free boundaries and high Rayleigh number it is possible to reproduce the observed magnitudes of the zonal and non‐zonal flow components at the surfaces of Jupiter and Saturn. While only three flow bands are found for a thick convecting shell, the number increases to seven for a shell with an inner‐to‐outer radius of 0.6.