Pedersen density drift instabilities
Creators
- 1. Earth and Space Sciences Division, University of California, Los Alamos National Laboratory
Description
This paper describes the linear kinetic theory of electrostatic drift instabilities driven by Pedersen and density drift velocities. The model uses a uniform magnetic field B = zB; a weak, uniform density gradient in the x direction; and a weak, uniform electric field in the y direction. Weak charged-neutral collisoins are represented by the addition of BGK model terms to the Vlasov equaiton. The resulting local dispersion equation is used to study the properties of the associated instabilities at ka/sub i/> or approx. =1 (where k is the wave number and a/sub i/ is the ion gyroradius). Results show that the E x B gradient drift instability at kai/sub a/approx. =1 may grow in the auroral ionosphere primarily in the vicinity of 200 km and only if the electron density is sufficiently small
Additional details
Publishing Information
- Journal Title
- J. Geophys. Res.
- Journal Volume
- 88
- Journal Issue
- A12
- Series
- J. Geophys. Res.
- Journal Page Range
- 10104-10110
- ISSN
- 0022-1406
INIS
- Country of Publication
- United States
- Country of Input or Organization
- United States
- INIS RN
- 15058625
- Subject category
- S58: GEOSCIENCES;
- Descriptors DEI
- DISPERSION RELATIONS; DRIFT INSTABILITY; ELECTRIC FIELDS; ELECTRON DENSITY; INSTABILITY GROWTH RATES; IONOSPHERE
- Descriptors DEC
- EARTH ATMOSPHERE; INSTABILITY; PLASMA INSTABILITY; PLASMA MICROINSTABILITIES