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引用次数: 0
摘要
摘要。本文结合欧姆加热模型和磁流体动力学动量方程,对电离层内的漂移和磁扰动模型进行了理论和数值研究。基于这些方程,研究了电离层电子温度和漂移电流。结果表明,电子温度的最大变化ΔTe约为570 K,比值为ΔTe/Te ~ 48%。最大漂移电流密度为8×10-10 A m−2,其表面积分为5.76 A。抗磁漂移电流是电流的主要形式。带电粒子与中性粒子的低碰撞频率对电流影响不大,电子与离子的碰撞频率与漂移电流无关。电流密度曲线是一个流动环。我们提出了有效电导率作为地磁场和无线电波之间夹角的函数;该模型解释了为什么当X波沿着磁倾角加热时辐射效率最强,正如Kotik等人(2013)最近的观测所报道的那样。根据MHD理论计算了加热区的磁场变化,结果表明加热区的磁场扰动最大为48 pT。
F-region drift current and magnetic perturbation distribution by the X-wave heating ionosphere
Abstract. We present a theoretical and numerical study of the drift current and magnetic perturbation model in the ionosphere by incorporating the ohmic heating model and the magnetohydrodynamic (MHD) momentum equation. Based on these equations, the ionospheric electron temperature and drift current are investigated. The results indicate that the maximum change in electron temperature ΔTe is about 570 K, and the ratio is ΔTe/Te ∼ 48 %. The maximum drift current density is 8×10-10 A m−2, and its surface integral is 5.76 A. Diamagnetic drift current is the main form of current. The low collision frequency between charged particles and neutral particles has little effect on the current, and the collision frequency of electrons and ions is independent of the drift current. The current density profile is a flow ring. We present the effective conductivity as a function of the angle between the geomagnetic field and the radio wave; the model explains why the radiation efficiency was strongest when the X wave is heating along the magnetic dip angle, as reported in recent observations by Kotik et al. (2013). We calculate the magnetic field variation in the heating region based on the MHD theory: the results show that the maximum magnetic field perturbation in the heating area is 48 pT.
期刊介绍:
Annales Geophysicae (ANGEO) is a not-for-profit international multi- and inter-disciplinary scientific open-access journal in the field of solar–terrestrial and planetary sciences. ANGEO publishes original articles and short communications (letters) on research of the Sun–Earth system, including the science of space weather, solar–terrestrial plasma physics, the Earth''s ionosphere and atmosphere, the magnetosphere, and the study of planets and planetary systems, the interaction between the different spheres of a planet, and the interaction across the planetary system. Topics range from space weathering, planetary magnetic field, and planetary interior and surface dynamics to the formation and evolution of planetary systems.