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Space weather effects on lower ionosphere: First investigation from Bharati station during 34th Indian scientific expedition to Antarctica

机译:太空天气对低层电离层的影响:第34届印度对南极的科学考察,巴拉蒂站的首次调查

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We investigate the solar flare effects on the D-region of the ionosphere with the help of VLF (Very Low Frequency) radio waves using a portable E-field system from Antarctica during the summer period of 34th Indian scientific expedition. Two GPS time synchronized VLF receivers, one located at Bharati, Antarctica (geographical latitude 69.40°S, longitude 76.18°E) and another located at Tripura, India (geographical latitude 23.84°N, longitude 91.28°E) were operated simultaneously to infer common mode changes in the lower ionosphere for a number of solar flares events. The two systems constantly monitored the carrier amplitude and phase of the MSK (Minimum Shift Keying) modulated navy transmitter located in Australia (Callsign: NWC, 19.8 kHz, geographical latitude 21.88°S, longitude 114.13°E), around 5.6 Mm great circle distance from the two receivers. The results are interpreted in terms of Earth-ionosphere wave-guide characteristics. A Long Wave Propagation Capability (LWPC) model study is also performed to infer the changes in the daytime electron density in polar D-region ionosphere during the solar flares. The exponential fit of the modeled electron density change with average X-ray flux change shows an excellent correlation (R2 value 0.95). The exponential fit is utilized to infer the daytime electron density change in the polar ionosphere during solar flare events. The analyses indicate that small solar flares of class 'C' can be very effectively detected with the portable antenna system even if the receiver is located in polar coastal region compared to equatorial region. The expedition results also demonstrate the feasibility of using portable VLF receivers from the coastal stations for monitoring the polar lower ionosphere from Antarctica and open up new opportunities for long term exploration.
机译:在第34届印度科学考察队的夏季,我们利用来自南极洲的便携式电子场系统,借助VLF(甚低频)无线电波,研究了电离层D区域太阳耀斑的影响。同时操作了两个GPS时间同步VLF接收机,一个位于南极Bharati(地理纬度69.40°S,东经76.18°E),另一个位于印度Tripura(地理纬度23.84°N,东经91.28°E),以推断共同点。在下层电离层中,许多太阳耀斑事件的模式改变。这两个系统不断监测位于澳大利亚的MSK(最小频移键控)调制海军发射机的载波幅度和相位(呼号:NWC,19.8 kHz,地理纬度21.88°S,经度114.13°E),大圆距离约为5.6 Mm来自两个接收器。根据地球电离层的波导特性来解释结果。还进行了长波传播能力(LWPC)模型研究,以推断太阳耀斑期间极地D区电离层中白天电子密度的变化。模拟的电子密度变化与平均X射线通量变化的指数拟合显示出极好的相关性(R2值为0.95)。指数拟合用于推断太阳耀斑事件期间极地电离层中白天电子密度的变化。分析表明,即使接收器位于赤道地区以外的极地沿海地区,也可以使用便携式天线系统非常有效地检测出“ C”级小太阳耀斑。考察结果还证明了使用沿海站的便携式VLF接收机监测南极极地电离层的可行性,并为长期勘探开辟了新的机会。

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