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首页> 外文期刊>Radiophysics and quantum electronics >GENERATION OF VLF EMISSIONS WITH THE INCREASING AND DECREASING FREQUENCY IN THE MAGNETOSPERIC CYCLOTRON MASER IN THE BACKWARD WAVE OSCILLATOR REGIME
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GENERATION OF VLF EMISSIONS WITH THE INCREASING AND DECREASING FREQUENCY IN THE MAGNETOSPERIC CYCLOTRON MASER IN THE BACKWARD WAVE OSCILLATOR REGIME

机译:后向波振荡系统中,随着磁控回旋环激磁频率的增加和减少,VLF辐射的产生

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We study the mechanisms of the formation of falling tones in the dynamic spectrum of whistler-mode waves generated by energetic electrons in the Earth's magnetosphere when the backward-wave oscillator (BWO) regime is realized in the magnetospheric cyclotron maser. As was shown earlier, this regime allows one to explain many features of ELF/VLF chorus emissions in the magnetosphere, in particular, the generation of elements with discrete frequency spectrum, characterized by a large growth rate and a fast frequency drift. On the basis of numerical simulations of a simplified system of nonlinear equations describing the magnetospheric BWO dynamics under the assumption of small efficiency of wave-particle interactions we show that the falling tones are generated in the case where the generation region is shifted from the equatorial plane (geomagnetic-field minimum) upstream with respect to the motion of energetic electrons. In this case, the resonant electrons move towards the decreasing magnetic field in the process of generation; hence, their longitudinal velocity increases, which corresponds to a decrease in the cyclotron-resonance frequency. Two mechanisms of the shift of the generation region from the equator are considered, i.e., (i) an increase in the linear instability growth rate (e. g., due to an increase in the energetic-electron density), and (ii) persistence of the phase bunching of the particles coming back to the generation region due to the bounce oscillations. We show that both of these mechanisms can result in the formation of falling tones, but the properties of the generated emissions such as the frequency drift rate and characteristic time interval between the elements are different. The conditions of preserving the phase bunching due to the bounce oscillations are discussed. Probably, this mechanism can operate in the case where the length of the generation region along the magnetic field is close to the characteristic bounce-oscillation length of energetic electrons which is realized for a sufficiently high cold-plasma density in the generation region.
机译:我们研究了当在磁层回旋加速器激射器中实现反向波振荡器(BWO)体制时,由地球磁层中高能电子产生的啸叫模式波的动态频谱中下降音的形成机理。如前所述,这种机制使人们可以解释磁层中ELF / VLF合唱发射的许多特征,特别是具有离散频谱的元素的生成,其特征在于大的增长率和快速的频率漂移。基于简化的描述磁层BWO动力学的非线性方程组的数值模拟,在波粒相互作用效率较低的假设下,我们表明,在生成区域偏离赤道平面的情况下,会产生下降的音调相对于高能电子的运动(最小地磁场)。在这种情况下,共振电子在生成过程中朝着逐渐减小的磁场移动。因此,它们的纵向速度增加,这与回旋共振频率的降低相对应。考虑了生成区域从赤道偏移的两种机制,即(i)线性不稳定性增长率的增加(例如,由于高能电子密度的增加),以及(ii)持续存在由于弹跳振荡,粒子的相位聚集回到生成区域。我们表明,这两种机制都可能导致音调下降,但是所产生的发射的特性(如频率漂移率和元素之间的特征时间间隔)不同。讨论了由于反弹振荡而保持相位聚束的条件。可能的是,该机制可以在沿着磁场的生成区域的长度接近高能电子的特征弹跳长度的情况下实现,该高能电子的特征是对于生成区域中足够高的冷等离子体密度实现的。

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