Formation, structure, and stability of MHD intermediate shocks
Description
Contrary to the usual belief that MHD intermediate shocks are extraneous, the author has recently shown by numerical solutions of dissipative MHD equations that intermediate shocks are admissible and can be formed through nonlinear wave steepening from continuous waves. In this paper, the formation, structure and stability of intermediate shocks in dissipative MHD are considered in detail. The differences between the conventional theory and his are pointed out and clarified. He shows that all four types of intermediate shocks can be formed from smooth waves. He also shows that there are free parameters in the structure of the intermediate shocks, and that these parameters are related to the shock stability. In addition, he shows that a rotational discontinuity can not exist with finite width, indicate how this is related to the existence of time-dependent intermediate shocks, and show why the conventional theory is not a good approximation to dissipative MHD solutions whenever there is rotation in magnetic field
Additional details
Publishing Information
- Journal Title
- Journal of Geophysical Research
- Journal Volume
- 95
- Journal Issue
- A6
- Series
- J. Geophys. Res.
- Journal Page Range
- 8149-8175
- ISSN
- 0148-0227
- CODEN
- JGREA
INIS
- Country of Publication
- United States
- Country of Input or Organization
- United States
- INIS RN
- 22089211
- Subject category
- S58: GEOSCIENCES;
- Descriptors DEI
- ALGORITHMS; MAGNETIC RECONNECTION; MAGNETOHYDRODYNAMICS; MAGNETOPAUSE; NAVIER-STOKES EQUATIONS; NONLINEAR PROBLEMS; NUMERICAL SOLUTION; SHOCK WAVES; STABILITY; TIME DEPENDENCE
- Descriptors DEC
- DIFFERENTIAL EQUATIONS; EQUATIONS; FLUID MECHANICS; HYDRODYNAMICS; MECHANICS; PARTIAL DIFFERENTIAL EQUATIONS