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Title: Oblique propagation of nonlinear hydromagnetic waves: One- and two-dimensional behavior

Abstract

The one- and two-dimensional behavior of obliquely propagating hydromagnetic waves is analyzed by means of analytical theory and numerical simulations. It is shown that the nonlinear evolution of a one-dimensional MHD wave leads to the formation of a rotational discontinuity and a compressive steepened quasi-linearly polarized pulse whose structure is similar to that of a finite amplitude magnetosonic simple wave. For small propagation angles, the pulse mode (fast or slow) depends on the value of {beta} with respect to unity while for large propagation angles the wave mode is fixed by the sign of the initial density-field correlation. The two-dimensional evolution shows that an MHD wave is unstable against a small-amplitude long-wavelength modulation in the direction transverse to the wave propagation direction. A two-dimensional magnetosonic wave solution is found, in which the density fluctuation is driven by the corresponding total pressure fluctuation, exactly as in the one-dimensional simple wave. Along with the steepening effect, the wave experiences both wave front deformation and a self-focusing effect which may eventually lead to the collapse of the wave. The results compare well with observations of MHD waves in the Earth's foreshock and at comets.

Authors:
 [1];  [2]
  1. Univ. della Calabria, Cosenza (Italy)
  2. Observatoire de Paris-Meudon (France)
Publication Date:
OSTI Identifier:
5186759
Resource Type:
Journal Article
Journal Name:
Journal of Geophysical Research; (United States)
Additional Journal Information:
Journal Volume: 96:A5; Journal ID: ISSN 0148-0227
Country of Publication:
United States
Language:
English
Subject:
71 CLASSICAL AND QUANTUM MECHANICS, GENERAL PHYSICS; HYDROMAGNETIC WAVES; WAVE PROPAGATION; ANALYTICAL SOLUTION; COMETS; COMPARATIVE EVALUATIONS; EARTH MAGNETOSPHERE; INTERACTIONS; IONS; MAGNETOACOUSTIC WAVES; NONLINEAR PROBLEMS; PLASMA DENSITY; REFLECTION; SOLAR WIND; WAVE FORMS; CHARGED PARTICLES; EARTH ATMOSPHERE; EVALUATION; SOLAR ACTIVITY; 640201* - Atmospheric Physics- Auroral, Ionospheric, & Magetospheric Phenomena; 640107 - Astrophysics & Cosmology- Planetary Phenomena

Citation Formats

Malara, F, and Elaoufir, J. Oblique propagation of nonlinear hydromagnetic waves: One- and two-dimensional behavior. United States: N. p., 1991. Web. doi:10.1029/90JA01588.
Malara, F, & Elaoufir, J. Oblique propagation of nonlinear hydromagnetic waves: One- and two-dimensional behavior. United States. https://doi.org/10.1029/90JA01588
Malara, F, and Elaoufir, J. 1991. "Oblique propagation of nonlinear hydromagnetic waves: One- and two-dimensional behavior". United States. https://doi.org/10.1029/90JA01588.
@article{osti_5186759,
title = {Oblique propagation of nonlinear hydromagnetic waves: One- and two-dimensional behavior},
author = {Malara, F and Elaoufir, J},
abstractNote = {The one- and two-dimensional behavior of obliquely propagating hydromagnetic waves is analyzed by means of analytical theory and numerical simulations. It is shown that the nonlinear evolution of a one-dimensional MHD wave leads to the formation of a rotational discontinuity and a compressive steepened quasi-linearly polarized pulse whose structure is similar to that of a finite amplitude magnetosonic simple wave. For small propagation angles, the pulse mode (fast or slow) depends on the value of {beta} with respect to unity while for large propagation angles the wave mode is fixed by the sign of the initial density-field correlation. The two-dimensional evolution shows that an MHD wave is unstable against a small-amplitude long-wavelength modulation in the direction transverse to the wave propagation direction. A two-dimensional magnetosonic wave solution is found, in which the density fluctuation is driven by the corresponding total pressure fluctuation, exactly as in the one-dimensional simple wave. Along with the steepening effect, the wave experiences both wave front deformation and a self-focusing effect which may eventually lead to the collapse of the wave. The results compare well with observations of MHD waves in the Earth's foreshock and at comets.},
doi = {10.1029/90JA01588},
url = {https://www.osti.gov/biblio/5186759}, journal = {Journal of Geophysical Research; (United States)},
issn = {0148-0227},
number = ,
volume = 96:A5,
place = {United States},
year = {Wed May 01 00:00:00 EDT 1991},
month = {Wed May 01 00:00:00 EDT 1991}
}