2019
DOI: 10.1029/2019ja026584
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Toward an Integrated View of Ionospheric Plasma Instabilities: 3. Explicit Growth Rate and Oscillation Frequency for Arbitrary Altitude

Abstract: General analytic expressions are derived for the growth rate γ and oscillation frequency in the ion frame ωr′ of unstable plasma waves generated by ionospheric plasma instabilities including the Farley‐Buneman instability (FBI) and the gradient‐drift instability (GDI). The explicit expressions are developed for arbitrary altitude and scales in the local approximation. Limits of applicability are carefully considered focusing on the dependence on the electron density gradients G=∇n/n and wavelengths λ. It is s… Show more

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Cited by 9 publications
(54 citation statements)
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“…Traditional FBI treatment, however, does not include an additional inertial effect associated with the 1− I −1 term in equation . In the F region, this factor is indeed strongly negative (i.e., stabilizing) at long wavelengths, but can also be positive (destabilizing) at shorter wavelengths (Makarevich, , their Figure 4). The above analysis shows that this destabilization occurs for supercritical convection.…”
Section: Convection and Gradient Thresholds In The Valley Regionmentioning
confidence: 99%
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“…Traditional FBI treatment, however, does not include an additional inertial effect associated with the 1− I −1 term in equation . In the F region, this factor is indeed strongly negative (i.e., stabilizing) at long wavelengths, but can also be positive (destabilizing) at shorter wavelengths (Makarevich, , their Figure 4). The above analysis shows that this destabilization occurs for supercritical convection.…”
Section: Convection and Gradient Thresholds In The Valley Regionmentioning
confidence: 99%
“…In this section, a general expression for the growth rate is analyzed focusing on behavior with altitude and plasma drift speed V E = E / B . A version of the general expression for the growth rate that describes fundamental ionospheric plasma instabilities including FBI and GDI for arbitrary altitude has been derived by Makarevich (, equation (32)) as γ=trueψ^νi1k2[]siri2VE2cos2()α+β()1I1Cs2+GVEfsiri2()1+I11+trueψ^()1+I1. …”
Section: Convection Threshold In the Transitional Valley Regionmentioning
confidence: 99%
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