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Propagation Characteristics and Generation Mechanism of ELF/VLF Hiss Observed at Low-latitude Ground Station (L = 1.17)

机译:低纬地面站(L = 1.17)观测到的ELF / VLF Hiss的传播特性和产生机理

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摘要

Extremely low frequency (ELF)/Very low frequency (VLF) hiss is whistler mode wave that interacts with energetic electrons in the magnetosphere. The characteristics features of ELF/VLF hiss observed at low latitude ground station Jammu (Geomag. lat. 22°16′ N, L=1.17) are reported. It is observed that most of hiss events first propagate in ducted mode along higher L-values (L = 4–5), after reaching lower edge of ionosphere excite the Earth-ionosphere waveguide and propagate towards equator to be received at low-latitude station Jammu. To understand the generation mechanism of ELF/VLF hiss, incoherent Cerenkov radiated power from the low-latitude and mid-latitude plasmasphere are evaluated. Considering this estimated power as an input for wave amplification through wave–particle interaction, the growth rate and amplification factor is evaluated which is too small to explain the observed wave intensity. It is suggested that some non-linear mechanism is responsible for the generation of ELF/VLF hiss.
机译:极低频(ELF)/极低频(VLF)嘶嘶声是一种惠斯勒模式波,它与磁层中的高能电子相互作用。报道了在低纬度地面站查((地球纬度22°16′N,L = 1.17)观测到的ELF / VLF hiss的特征。可以看到,大多数嘶嘶声事件首先到达高电离层的低边缘(L = 4-5),然后沿高L值以管道模式传播,然后激发地球-电离层波导并向赤道传播,并在低纬度站被接收查mu为了了解ELF / VLF嘶嘶声的产生机理,对低纬度和中纬度等离子层的不相干切伦科夫辐射功率进行了评估。将该估算的功率视为通过波粒相互作用进行波放大的输入,因此评估了增长率和放大因子,该值太小而无法解释观察到的波强度。建议某种非线性机制负责ELF / VLF嘶嘶声的产生。

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