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低电离层舒曼谐振观测

曹丙霞 乔晓林

曹丙霞, 乔晓林. 低电离层舒曼谐振观测[J]. 电子与信息学报, 2010, 32(8): 2002-2005. doi: 10.3724/SP.J.1146.2009.01535
引用本文: 曹丙霞, 乔晓林. 低电离层舒曼谐振观测[J]. 电子与信息学报, 2010, 32(8): 2002-2005. doi: 10.3724/SP.J.1146.2009.01535
Cao Bing-Xia, Qiao Xiao-Lin. Observations on Schumann Resonance in Low Ionosphere[J]. Journal of Electronics & Information Technology, 2010, 32(8): 2002-2005. doi: 10.3724/SP.J.1146.2009.01535
Citation: Cao Bing-Xia, Qiao Xiao-Lin. Observations on Schumann Resonance in Low Ionosphere[J]. Journal of Electronics & Information Technology, 2010, 32(8): 2002-2005. doi: 10.3724/SP.J.1146.2009.01535

低电离层舒曼谐振观测

doi: 10.3724/SP.J.1146.2009.01535
基金项目: 

国家科技支撑计划项目(2008BAC35B00)资助课题

Observations on Schumann Resonance in Low Ionosphere

  • 摘要: 舒曼谐振与大气温度变化及地震电磁前兆密切相关,该文针对地面直接观测受环境制约严重的问题,提出了一种新的舒曼谐振监测方法,即人工向电离层发射高频(HF)电磁波,与舒曼谐振产生电离层交叉调制,通过解调HF波获得舒曼谐振。基于大气晴天电场作用下HF电磁波与舒曼谐振在低电离层的非线性调制模型,论证了该方法的可行性;利用我国首个舒曼谐振观测台站,接收短波授时信号BPM,并在其解调谱图上得到了分别位于7 Hz,14 Hz,20 Hz,26 Hz的舒曼谐振前4阶谐振峰。理论及实验表明在HF的解调谱上获取低电离层舒曼谐振,是一种可行的舒曼谐振观测方式。
  • Schumann W O. ber die ausbreitung sehr langerelektriseher wellen um die signale des blitzes. Nuovo Cimento1952, 9(12): 1116-1138.[2]Morente J A, Port J A, and Salinas A, et al.. Evidence ofelectrical activity on titan drawn from the schumannresonances sent by huygens probe. International Journal ofSolar System Studies, 2008, 195(2): 802-811.[3]Nieckarz Z, Kulak A, and Zieba S, et al.. Comparison ofglobal storm activity rate calculated from schumannresonance background components to electric field intensityE0Z[J].Atmospheric Research.2009, 91(2-4):184-187[4]Hayakawa M, Nickolaenko A P, and Sekiguchi M, et al..Anomalous elf phenomena in the schumann resonance bandas observed at moshiri (japan) in possible association with anearthquake in taiwan[J].Natural Hazards and Earth SystemSciences.2008, 8(6):1309-1316[5]Ohta K, Izutsu J, and Hayakawa M. Anomalous excitation ofschumann resonances and additional anomalous resonancesbefore the 2004 mid-niigata prefecture earthquake and the2007 noto hantou earthquake[J].Physics and Chemistry of theEarth, Parts A/B/C.2009, 34(6-7):441-448[6]Ohta K, Watanabe N, and Hayakawa M, et al..Electromagnetic fields and schumann resonance on taiwaiearthquakes. in Electromagnetic Compatibility 2004, 17thInternational Wroclaw Symposium and Exhibition. Poland,2004.[7]Ohta K,Watanabe N, and Hayakawa M. Survey of anomalousschumann resonance phenomena observed in japan, inpossible association with earthquakes in taiwan[J].Physics andChemistry of the Earth, Parts A/B/C.2006, 31(4-9):397-402[8]Hayakawa M, Ohta K, and Nickolaenko A P, et al..Anomalous effect in schumann resonance phenomenaobserved in japan, possibly associated with the chi-chiearthquake in taiwan[J].Annales Geophysicae.2005, 23(4):1335-1346[9]Nickolaenko A P, Hayakawa M, and Sekiguchi M, et al..Model modifications in schumann resonance intensity causedby a localized ionosphere disturbance over the earthquakeepicenter[J].Annales Geophysicae.2006, 24(2):567-575[10]曹丙霞, 乔晓林. 基于地球-电离层空腔共振的地震电磁监测方法研究. 国际地震动态, 2009, (7): 22-26.[11]Alpert Y L. Propagation of electromagnetic waves and theionosphere. Nauka, 1972, 1(1): 563.[12]Yampolski Y M, Bliokh P V, and Beley V S, et al.. Non-linearinteraction between schumann resonances and hf signals[J].Journal of Atmospheric and Solar-Terrestrial Physics.1997,59(3):335-342[13]Nickolaenko A P and Hayakawa M. Resonances in the Earth-Ionosphere Cavity. Netherlands: Kluwer Academic Publishers.2002: 156-169.[14]Gurevich A V. Nonlinear Phenomena in the Ionosphere. NewYork: Springer. 1978: 113-114.[15]肖景明, 王元坤. 电波传播工程计算. 西安: 西安电子科技大学出版社, 1989: 47-48.
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出版历程
  • 收稿日期:  2009-12-10
  • 修回日期:  2010-04-16
  • 刊出日期:  2010-08-19

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