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Data · dataset · 2026

Three-dimensional magneto-shear instabilities in the solar tachocline - II. Axisymmetric case

Listed in National Center for Atmospheric Research

A Boussinesq model of the development of non-axisymmetric (in particular m= 1) three-dimensional magneto-shear instabilities in the solar tachocline was presented in Paper I. However, there it was erroneously concluded that the axisymmetric (m= 0) modes are stable, and they were not discussed further.

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Here it is shown that, although m= 0 modes are indeed stable for broad magnetic profiles, they are strongly unstable to radial shredding (high radial wavenumber) instabilities on the poleward shoulders of toroidal magnetic bands at high field strengths (roughly 40-100 kG depending on bandwidth and latitude).

These instabilities have growth rates comparable to or greater than those for tipping instabilities (m= 1) in many cases, but both are strongly stabilized by gravitational stratification characteristic of the upper radiative core. Weaker fields are m= 0 stable (though weakly m= 1 unstable), even in neutral gravitational stratification (convection zone).

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Provenance · 1 source records, 7 field assertions
SourceKeyLast seenRaw
National Center for Atmospheric Researche4521470-751a-485c-9d06-77a72ca47ec412 d agoJSON v1
FieldAssertionExtractorEvidence
concepts[field].local:field:earth-environmentalmapping · data ucar educonnector:data_ucar_edu@1.0.0
concepts[field].local:field:ocean-atmosphericmapping · data ucar educonnector:data_ucar_edu@1.0.0
created_datesource · data ucar educonnector:data_ucar_edu@1.0.0
descriptionsource · data ucar educonnector:data_ucar_edu@1.0.0/notes
publication_datesource · data ucar educonnector:data_ucar_edu@1.0.0
titlesource · data ucar educonnector:data_ucar_edu@1.0.0/title
updated_datesource · data ucar educonnector:data_ucar_edu@1.0.0