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首页> 外文期刊>Journal of atmospheric and solar-terrestrial physics >Meteor-head echo observations using an antenna compression approach with the 450 MHz Poker Flat Incoherent Scatter Radar
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Meteor-head echo observations using an antenna compression approach with the 450 MHz Poker Flat Incoherent Scatter Radar

机译:使用天线压缩方法和450 MHz Poker Flat非相干散射雷达进行流星头回波观测

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In this work we present a novel use of the Poker Flat Incoherent Scatter Radar (PFISR) to study meteor-head echoes with wide (W) beams. Until now, most of the meteor-head echo studies have been performed with High-Power Large-Aperture Radars (HPLARs) using very narrow (N) beams. At PFISR we have implemented an antenna compression approach using a defocusing scheme, similar to Chirp (linear frequency modulation) in pulse compression. The resulting effective beam is similar to 3 times wider than the narrowest PFISR beam. Using the signal-to-noise ratio (SNR) as a proxy measurement of cross-section, from the combined W and N beam experiments, our main results are: (1) observed meteors in the W beam are approximately half the number of meteors observed in the N beam, (2) we detected 10 times more large cross-section (strong) meteors (> 15 dB if they were measured by the N mainlobe) than using only the N beam, and (3) more than 15% of the total N meteors were observed in the N sidelobes, therefore being at least 20 dB stronger if they were observed in the N mainlobe. Our results are summarized in a corrected distribution of relative meteor cross-sections as if all of them were observed with the N mainlobe, namely correcting their SNR values depending on where in the beam they were detected (sidelobes or mainlobe). in addition, we show a qualitative meteor cross-section distribution that one can obtain combining W and N beams. The resulting distribution is incomplete, since the W beam is not sensitive enough to detect the very small (weak) meteors, but could provide new information about the large cross-section events.
机译:在这项工作中,我们提出了一种新颖的使用扑克平面非相干散射雷达(PFISR)来研究宽(W)光束流星头回声的方法。到目前为止,大多数流星回声研究都是使用大功率大孔径雷达(HPLAR)使用非常窄的(N)波束进行的。在PFISR,我们使用散焦方案实现了天线压缩方法,类似于脉冲压缩中的Chirp(线性频率调制)。产生的有效光束大约是最窄PFISR光束的3倍。使用信噪比(SNR)作为横截面的替代测量,通过组合的W和N​​束实验,我们的主要结果是:(1)在W束中观察到的流星大约是流星数量的一半在N光束中观察到的结果,(2)我们检测到的大横截面(强)流星(如果由N主瓣测量则大于15 dB)比仅使用N光束大10倍,(3)大于15%在N个旁瓣中观测到N个流星总数的一半,因此,如果在N个主瓣中观测到它们,则流星的强度至少要强20 dB。我们的结果总结为相对流星横截面的校正分布,就好像它们都是用N个主瓣观察到的一样,即根据检测到的波束中的位置(旁瓣或主瓣)校正其SNR值。此外,我们显示了定性的流星横截面分布,可以得到W和N光束的组合。由于W光束不够灵敏,无法检测到非常小的(弱)流星,但可以提供有关大截面事件的新信息,因此所得的分布不完整。

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