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出 处:《地球物理学报》2009年第3期599-606,共8页Chinese Journal of Geophysics
基 金:国家自然科学基金项目(40374059)资助
摘 要:Alfven 波在低纬地区电离层的传播有其特殊性。一方面,低纬地区同样存在 Alfven 速度梯度的巨大变化.导致电离层 Alfven 谐振器(Ionospheric Alfven resonator,IAR)的形成;另一方面,由于在低纬地区磁倾角很小.所以剪切 Alfven 波在传播的过程中纬度方向跨度很大,不同纬度电离层参数将共同对其产生影响;并且,由于电离层水平分层,故磁力线与电离层不正交.本文选取双流体力学模型,在忽略场向电场的条件下.利用非正交坐标系,结合 IRI07模型与 MSISE00模型模拟低纬地区 Alfven 波的传播,得到其反射及耦合特性.结果表明,低纬地区同样存在电离层 Alfven 谐振现象,由耦合产生的压缩模有向磁赤道方向传播的趋势,夜间电离层状态相对于白天更适合 IAR 的形成,谐振频率沿磁力线 L 值增大单调递增.Alfven waves propagating in the low-latitude ionosphere exhibit particular characteristics. Firstly, sharp Alfven wave velocity gradient in the lowqatitude ionosphere introduces ionospheric Alfven resonator (IAR). Secondly, shear Alfven waves can propagate over a long distance at the latitude direction due to the small magnetic inclination angle, and the propagation properties of Alfven waves can be affected by the ionospheric parameters at different latitudes. Thirdly, the low-latitude magnetic field lines are oblique to the ionosphere which is horizontally isotropic. In absence of the field aligned electric field and by use of IRI07 model and MSISE00 model, a two- fluid momentum model based on non-orthogonal coordinate system is used to simulate the characteristics of Alfven wave propagation, reflection, and coupling. The results indicate that IAR can also occur in the low-latitude ionosphere, and compressional mode excited by coupling with shear mode is likely to diffuse to the magnetic equator. It is also found that IAR tends to occur more frequently at nighttime than daytime with the resonance frequency increasing with the L-shell.
分 类 号:P352[天文地球—空间物理学]
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