Long wavelength limit of the current convective instability
Journal Article
·
· J. Geophys. Res.; (United States)
A linear theory is presented of the current convective instability in the long wavelength limit, i.e., kL<<1 where k is the wave number and L is the scale length of the density inhomogeneity A relatively simple dispersion equation is derived that describes the modes in this limit. Analytical solutions are presented in both the collisional (..nu../sub i/n>>..omega..) and inertial (..nu../sub i/n>>..omega..) limits where ..omega.. is the wave frequency and ..nu../sub i/n is the ion-neutral collision frequency. It is shown that the growth rate scales as k in the collisional limit and as k/sup 2/3/ in the inertial limit. The analytical solutions are compared to exact numerical solutions, and very good agreement is found. Applications to the auroral ionosphere are discussed.
- Research Organization:
- Geophysical and Plasma Dynamics Branch, Plasma Physics Division, Naval Research Laboratory
- OSTI ID:
- 6653161
- Journal Information:
- J. Geophys. Res.; (United States), Journal Name: J. Geophys. Res.; (United States) Vol. 89:A5; ISSN JGREA
- Country of Publication:
- United States
- Language:
- English
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Related Subjects
640201* -- Atmospheric Physics-- Auroral
Ionospheric
& Magetospheric Phenomena
71 CLASSICAL AND QUANTUM MECHANICS
GENERAL PHYSICS
ANALYTICAL SOLUTION
COLLISIONS
CONVECTIVE INSTABILITIES
DIMENSIONS
DISPERSION RELATIONS
EARTH ATMOSPHERE
HEIGHT
INSTABILITY
INSTABILITY GROWTH RATES
ION COLLISIONS
ION-MOLECULE COLLISIONS
IONOSPHERE
MOLECULE COLLISIONS
NUMERICAL SOLUTION
PLANETARY IONOSPHERES
PLASMA DENSITY
PLASMA INSTABILITY
SCALE HEIGHT
Ionospheric
& Magetospheric Phenomena
71 CLASSICAL AND QUANTUM MECHANICS
GENERAL PHYSICS
ANALYTICAL SOLUTION
COLLISIONS
CONVECTIVE INSTABILITIES
DIMENSIONS
DISPERSION RELATIONS
EARTH ATMOSPHERE
HEIGHT
INSTABILITY
INSTABILITY GROWTH RATES
ION COLLISIONS
ION-MOLECULE COLLISIONS
IONOSPHERE
MOLECULE COLLISIONS
NUMERICAL SOLUTION
PLANETARY IONOSPHERES
PLASMA DENSITY
PLASMA INSTABILITY
SCALE HEIGHT