摘要
本文研究了0.1～10 Hz频率范围内的ULF波从磁层到地面的传播,得到了解析解,分析了电离层Alfven谐振器、磁倾角、电离层电导率、以及波频率对地面观测到的地磁信号的影响.数值结果表明:在磁层中剪切波在竖直方向有明显的谐振结构;地面观测到的信号在IAR谐振频率出现极大值,其谐振频率随磁倾角的增大而增大;电离层电导率的变化可以改变IAR的谐振频率,并能改变波的透射,从而影响地面地磁信号的频谱.
The propagation of ULF waves in the Pcl range （0.1-10 Hz） from magnetosphere to ground is examined in the presence of oblique background magnetic fields. The analytic solution is derived to analyze the influences of the ionospheric Alfven resonator （IAR）, conductivities, and the frequency of the ULF waves on the geomagnetic signal. The results of the numerical calculation show that the shear mode exhibits resonant structure vertically; the geomagnetic signal reaches its peak at the IAR resonant frequencies which increase with dip angle; the variation of Hall conductivity leads to the modulation of IAR resonant frequencies and the transmission of the ULF waves which effectively influence the spectrum of geomagnetic signal at ground.
出处
《地球物理学报》
SCIE
EI
CAS
CSCD
北大核心
2010年第9期2013-2022,共10页
Chinese Journal of Geophysics
基金
国家自然科学基金项目(40890164,40974083,41004061,41031064)
国家科技支撑计划课题(2006CB806306)
极地科学青年创新基金(JDQ200905)资助
