Abstract

In this pa per, a two-dimensional numerical study of a plasma density gradient effect on Farley-Buneman waves (FB waves) is per formed via a two-fluid code in which the electron inertia is neglected while the ion inertia is retained. We focused the simulations on the interaction between a single wave mode and the back ground E region where the vertical density gradient profile and the weaker than FB threshold ambient electric field were considered. From 2D density contour maps, it was found that the FB wave grows in the region of ▽N(subscript e)•E>0(where ▽N(subscript e) is the electron density gradient and E is the electric field), the initial growth rate was in reason able agreement with the prediction of the combined linear theory of Farley-Buneman and gradient drift instabilities, and the propagation speed was modulated by the gradient strength. Ac cording to the phase velocity evaluated by the Fourier analysis and peak to peak estimation method, the density gradients were found to have an effect of lowering the phase velocity at saturation, which is smaller than ion-acoustic speed for large scale waves, and the results demonstrated that the reduction of phase velocity by a density gradient effect was larger for a longer wave length wave than shorter wave length curve. It was also found that the plausible density gradient effects seem to be related to the thickness of the density gradient region and vertical electric field where the FB wave was traveling. The thicker unstable layer would cause a greater phase velocity reduction than the thinner unstable layer might cause, and the large driving electric field would reduce the wavelength dependence of density gradient effect on the saturation phase velocity.

Highlights

  • The existence of plasma waves in the E region has been known for several decades

  • Following the combined linear theory of Farley-Buneman and gradient-drift (FB-GD) instabilities, if the density gradients exist along the ambient electric field which is slightly weaker than the FB instability threshold electric field, the short-scale FB waves can still be excited directly

  • We have carried out 2D simulations of density gradient effects on the phase velocity at saturation of two-stream waves

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Summary

INTRODUCTION

The existence of plasma waves in the E region has been known for several decades. Numerous studies on those plasma waves have led to a conclusion that the mechanisms generating the plasma waves demonstrate Farley-Buneman (FB) and the gradient-drift (GD) instabilities (e.g., see Fejer and Kelley 1980; Farley 1985; Kelley 1989). Chi-Lon Fern & Fu-Shong Kuo on type 1 waves was presented by Hanuise and Crochet (1981), who found the lower type 1 Doppler velocities as their radar observation shifted from higher to lower radar frequencies They attributed the lower instability thresholds to a destabilized ambient plasma density gradient. They pointed out that the other statistical HF radar studies in the aurora region (e.g., Hanuise et al 1991; Milan et al 1997; Milian and Lester 2001; Lacroix and Moorcroft 2001) had reached the same conclusion Their studies had focused on the shorter scale FB waves of wavelengths of 1 and 3.15 m, and the relevant HF radar observations were located in the aurora region with a strong electric field, where some physical mechanisms are still not completely understood and clearly need more accurate study using more precise techniques including numerical simulation. NUMERICAL MODEL FOR DENSITY GRADIENT EFFECTS ON FARLEY-BUNEMAN WAVES

Numerical Model and Method of Data Analysis
A Test of the Numerical Model Using the Linear FB-GD Instability Theory
The Behavior of a Longer Wavelength Wave
The Saturation Simulations Associated with Gradient Effect
Simulations for Gradient Effects Related to 2D Structure of FB Waves
Simulations for Gradient Effect Related to Strong Electric Field
SUMMARY AND DISCUSSION
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