首页> 外文会议>Asian conference on remote sensing;ACRS >MATLAB-BASED VHF AND UHF AMPLITUDE SCINTILLATION CHARACTERIZATION USING THE NEW LOW-LATITUDE IONOSPHERIC TOMOGRAPHY NETWORK (LITN)
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MATLAB-BASED VHF AND UHF AMPLITUDE SCINTILLATION CHARACTERIZATION USING THE NEW LOW-LATITUDE IONOSPHERIC TOMOGRAPHY NETWORK (LITN)

机译:基于新型低纬度电离层层析成像网络(LITN)的基于MATLAB的VHF和UHF振幅闪烁表征

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The new LITN network was established in 2006 to study equatorial anomaly dynamics (Hsiao et al., 2009). It has ten Ionospheric Tomography Stations (ITS) placed along the 120°E longitude with stations in Japan, Taiwan, Philippines and Indonesia. These stations independently receive mutually coherent signals at VHF (150 MHz) and UHF (400 MHz) bands, which come from NNSS-like satellites and FORMOSAT-3/COSMIC satellites. Local ionospheric irregularities, that cause rapid fluctuations in radio signals or scintillation, can be studied using the total electron content (TEC) values acquired from the ITS receiver. In this study, a MATLAB-based application was developed to process these data for automatic identification and characterization of amplitude scintillation where six criteria are set to characterize an event as scintillation including the S_4 index, elevation angle, transmitting satellite, confirmation from other data recording and ground stations, and location difference of the recordings. LITN data was obtained from August 2008 to February 2011. Scintillation varied with operating frequency, local time, geographical location, solar activity and magnetic activity. Strong scintillation occurred more in VHF than in UHF. Moreover, nighttime scintillations occurred predominantly around local midnight (2000~0200 LT), while most of the daytime scintillation occurred at 0800~1000 LT. Scintillation mostly occurred between 15°-25° of geomagnetic latitude and almost none below 10° and above 30° geomagnetic latitude. Generally, the scintillation occurred under quiet magnetic condition and the occurrence increases as the solar activity increases.
机译:新的LITN网络建立于2006年,用于研究赤道异常动力学(Hsiao等,2009)。它在120°E的经度上设有10个电离层断层摄影站(ITS),分别位于日本,台湾,菲律宾和印度尼西亚。这些站在VHF(150 MHz)和UHF(400 MHz)频段上独立接收相互相干的信号,这些信号来自类似NNSS的卫星和FORMOSAT-3 / COSMIC卫星。可以使用从ITS接收器获得的总电子含量(TEC)值来研究导致电波信号或闪烁快速波动的局部电离层不规则性。在这项研究中,开发了一个基于MATLAB的应用程序来处理这些数据,以自动识别和表征振幅闪烁,其中设置了六个标准来将事件表征为闪烁,包括S_4指数,仰角,发射卫星,其他数据记录的确认和地面站,以及录音的位置差异。 LITN数据是从2008年8月到2011年2月获得的。闪烁的频率随工作频率,当地时间,地理位置,太阳活动和磁活动而变化。在VHF中发生的强闪烁比在UHF中发生的闪烁多。此外,夜间闪烁主要发生在当地午夜(2000〜0200 LT)左右,而白天大部分闪烁发生在0800〜1000 LT。闪烁主要发生在地磁纬度15°-25°之间,低于10°和高于30°地磁纬度几乎没有。通常,闪烁发生在安静的磁性条件下,并且随着太阳活动的增加而增加。

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