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Gradient drift instability as a source of spread F in the region of large-scale irregularities in the low-latitude topside ionosphere

机译:低纬顶电离层大尺度不规则区域中梯度漂移的不稳定性是扩散F的来源

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摘要

The expression for the increment of instability and decrement of diffusion damping of gradient drift waves for ionospheric altitudes above the F^sub 2^ layer maximum is obtained. The gradient drift instability is used to interpret the observations of spread F in the region of large-scale horizontal irregularities of the electron density. Two types of such irregularities observed on board the Intercosmos-19 (IC-19) satellite in the region of low latitudes (a peak of the density in the dusk ionosphere and a trough of the density in the dawn ionosphere) are considered. It is shown that the observed gradients of the density and electric field values in the dawn and dusk ionospheric sectors are quite sufficient for the instability development criterion to be satisfied in both considered cases. [PUBLICATION ABSTRACT]
机译:得到了电离层高度高于F ^ sub 2 ^层最大值时梯度漂移波的不稳定性增加和扩散阻尼减小的表达式。梯度漂移不稳定性用于解释在电子密度的大规模水平不规则区域中扩展F的观测结果。考虑了在低纬度地区的Intercosmos-19(IC-19)卫星上观测到的两种此类不规则性(黄昏电离层的密度峰值和黎明电离层的密度谷)。结果表明,在黎明和黄昏电离层中观测到的密度和电场值的梯度足以满足两种情况下的不稳定性发展标准。 [出版物摘要]

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