On the predominance of oblique disturbances in the supersonic shear flow instability of the geomagnetic tail boundary

A study is made of the influence of the longitudinal magnetic field and density inhomogeneity on the supersonic shear flow instability at the magnetospheric tail boundary. It is shown that the most unstable are slow oblique (3D) disturbances, with a phase velocity approaching at a sufficiently l...

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Main Author: V. V. Mishin
Format: Article
Language:English
Published: Copernicus Publications 2003-01-01
Series:Nonlinear Processes in Geophysics
Online Access:http://www.nonlin-processes-geophys.net/10/351/2003/npg-10-351-2003.pdf
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spelling doaj-3045779a80884d9e8a9d47819aa99fa12020-11-24T23:11:21ZengCopernicus PublicationsNonlinear Processes in Geophysics1023-58091607-79462003-01-01104/5351361On the predominance of oblique disturbances in the supersonic shear flow instability of the geomagnetic tail boundaryV. V. MishinA study is made of the influence of the longitudinal magnetic field and density inhomogeneity on the supersonic shear flow instability at the magnetospheric tail boundary. It is shown that the most unstable are slow oblique (3D) disturbances, with a phase velocity approaching at a sufficiently large angle (with respect to the flow direction) the magnetosonic velocity. Their growth rate and spectral width are much larger than those of the usually considered longitudinal (2D) supersonic disturbances. The magnetic field reduces the compressibility effect and, unlike the subsonic case, has a noticeable destabilizing effect on the excitation of oblique disturbances.http://www.nonlin-processes-geophys.net/10/351/2003/npg-10-351-2003.pdf
collection DOAJ
language English
format Article
sources DOAJ
author V. V. Mishin
spellingShingle V. V. Mishin
On the predominance of oblique disturbances in the supersonic shear flow instability of the geomagnetic tail boundary
Nonlinear Processes in Geophysics
author_facet V. V. Mishin
author_sort V. V. Mishin
title On the predominance of oblique disturbances in the supersonic shear flow instability of the geomagnetic tail boundary
title_short On the predominance of oblique disturbances in the supersonic shear flow instability of the geomagnetic tail boundary
title_full On the predominance of oblique disturbances in the supersonic shear flow instability of the geomagnetic tail boundary
title_fullStr On the predominance of oblique disturbances in the supersonic shear flow instability of the geomagnetic tail boundary
title_full_unstemmed On the predominance of oblique disturbances in the supersonic shear flow instability of the geomagnetic tail boundary
title_sort on the predominance of oblique disturbances in the supersonic shear flow instability of the geomagnetic tail boundary
publisher Copernicus Publications
series Nonlinear Processes in Geophysics
issn 1023-5809
1607-7946
publishDate 2003-01-01
description A study is made of the influence of the longitudinal magnetic field and density inhomogeneity on the supersonic shear flow instability at the magnetospheric tail boundary. It is shown that the most unstable are slow oblique (3D) disturbances, with a phase velocity approaching at a sufficiently large angle (with respect to the flow direction) the magnetosonic velocity. Their growth rate and spectral width are much larger than those of the usually considered longitudinal (2D) supersonic disturbances. The magnetic field reduces the compressibility effect and, unlike the subsonic case, has a noticeable destabilizing effect on the excitation of oblique disturbances.
url http://www.nonlin-processes-geophys.net/10/351/2003/npg-10-351-2003.pdf
work_keys_str_mv AT vvmishin onthepredominanceofobliquedisturbancesinthesupersonicshearflowinstabilityofthegeomagnetictailboundary
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