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首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >Effects of themajor sudden stratospheric warming event of 2009 on the subionospheric very low frequency/low frequency radio signals
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Effects of themajor sudden stratospheric warming event of 2009 on the subionospheric very low frequency/low frequency radio signals

机译:2009年主要突然平流层变暖事件对亚电离层非常低频/低频无线电信号的影响

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This paper presents effects of the major sudden stratospheric warming (SSW) event of 2009 on the subionospheric very low frequency/low frequency (VLF/LF) radio signals propagating in the Earth-ionosphere waveguide. Signal amplitudes from four transmitters received by VLF/LF radio networks of Germany and Japan corresponding to the major SSW event are investigated for possible anomalies and atmospheric influence on the high- to middle-latitude ionosphere. Significant anomalous increase or decrease of nighttime and daytime amplitudes of VLF/LF signals by -3-5 dB during the SSW event have been found for all propagation paths associated with stratospheric temperature rise at 10 hPa level. Increase or decrease in VLF/LF amplitudes during daytime and nighttime is actually due to the modification of the lower ionospheric boundary conditions in terms of electron density and electron-neutral collision frequency profiles and associated modal interference effects between the different propagating waveguide modes during the SSW period. TIMED/SABER mission data are also used to investigate the upper mesospheric conditions over the VLF/LF propagation path during the same time period. We observe a decrease in neutral temperature and an increase in pressure at the height of 75-80 km around the peak time of the event. VLF/LF anomalies are correlated and in phase with the stratospheric temperature and mesospheric pressure variation, while minimum of mesospheric cooling shows a 2-3 day delay with maximum VLF/LF anomalies. Simulations of VLF/LF diurnal variation are performed using the well-known Long Wave Propagating Capability (LWPC) code within the Earth-ionosphere waveguide to explain the VLF/LF anomalies qualitatively.
机译:本文介绍了2009年主要突然平流层变暖(SSW)事件对地球电离层波导传播的亚亚底椎间的非常低频/低频(VLF / LF)无线电信号的影响。由德国VLF / LF无线电网络接收的四个发射器的信号幅度对应于主要SSW事件的德国和日本进行对应于高纬度电离层的可能性异常和大气影响。对于在10HPa水平的平坦振温相关联的所有传播路径,发现了在SSW事件中的VLF / LF信号的夜间和白天和白天和白天幅度的显着增加或减少。白天和夜间VLF / LF幅度的增加或减少实际上是由于在电子密度和电子 - 中性碰撞频率分布方面改变了较低的电离层边界条件以及在SSW期间不同传播波导模式之间的相关模态干扰效应时期。定时/ SABER任务数据还用于在同一时间段内研究VLF / LF传播路径上的上部MESOSPERIC条件。我们观察中性温度的减少,在事件的峰值时间周围75-80 km的高度增加压力。 VLF / LF异常是相关的,并且具有平流层温度和伴曲性压力变化的相位,而Mesospheric冷却的最小值显示出2-3天的延迟,最大VLF / LF异常。使用地球电离层波导内的众所周知的长波传播能力(LWPC)代码进行VLF / LF昼夜变化的模拟,以定性地解释VLF / LF异常。

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