Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

HYDROMAGNETIC KELVIN-HELMHOLTZ INSTABILITY SURFACE WAVES AND GEOMAGNETIC MICROPULSATIONS. Final Report

Technical Report ·
OSTI ID:4712402
The most general form of hydromagnetic KelvinHelmholtz discontinuity in ideal incompressible fluids was considered. The stability of the hydromagnetic flow of two uniform infinite streams with planar interface exhibiting this type of discontinuity was analyzed in detail. Necessary criteria for its stability were obtained. A disturbance of the stable interface propagates as hydromagnetic surface waves. Instability of the interface leads to growing surface waves. A new theory is developed of geomagnetic micropulsations, in which the solar windexosphere interface is viewed as a surface of hydromagnetic Kelvin-Helmholtz discontinuity. The sunlit side of this interface is unstable under most conditions of solar activity. In the course of this work, a critical examination of the single fluid approximations of the plasma equations was made. A rigorous derivation of the boundary conditions in an ideal incompressible hydromagnetic fluid is given. 66 references. (auth)
Research Organization:
Columbia Univ., New York. School of Engineering
NSA Number:
NSA-17-018289
OSTI ID:
4712402
Report Number(s):
AFOSR-2764; AD-283988; CU-20-6
Country of Publication:
United States
Language:
English

Similar Records

Stability of Hydromagnetic Kelvin-Helmholtz Discontinuity
Journal Article · Mon Dec 31 23:00:00 EST 1962 · Physics of Fluids (New York) · OSTI ID:4677656

Kelvin-Helmholtz instability and the variation of geomagnetic pulsation activity
Journal Article · Wed Oct 01 00:00:00 EDT 1980 · Geophys. Res. Lett.; (United States) · OSTI ID:6878681

Destabilizing effect of density gradient on the Kelvin-Helmholtz instability
Journal Article · Sat Nov 14 23:00:00 EST 2009 · Physics of Plasmas · OSTI ID:21274239