首页> 外文会议>International Geoscience and Remote Sensing Symposium >INVESTIGATION OF IONOSPHERIC SCINTILLATION OVER SOUTH AFRICA AND THE SOUTH ATLANTIC ANOMALY USING GPS SIGNALS: FIRST RESULTS
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INVESTIGATION OF IONOSPHERIC SCINTILLATION OVER SOUTH AFRICA AND THE SOUTH ATLANTIC ANOMALY USING GPS SIGNALS: FIRST RESULTS

机译:使用GPS信号对南非和南大西洋异常进行电离层闪烁的调查:第一个结果

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Transionospheric radio communications and radio signals reflected from the Earth's ionosphere can be degraded when irregularities in the electron density of the ionosphere cause rapid variations in the amplitude and phase of such signals. Signals from GPS satellites which undergo scintillations can be used to characterise the location and extent of ionospheric scintillations and improve models for the prediction of ionospheric scintillations. The region in the South Atlantic Ocean where the Earth's magnetic field is weakest, known as South Atlantic Magnetic Anomaly (SAMA), is potentially a region where ionospheric scintillation may be more severe due to the precipitation of high energy particles from the Earth's radiation belts. This paper presents some of the first ionospheric scintillations observed by means of GPS signals received by dedicated scintillation monitors deployed in the mid-and auroral latitudes of the Southern Hemisphere since 2007.
机译:当电离层的电子密度的不规则性导致这种信号的幅度和相位的快速变化时,从地球电离层反射的转换层的无线电通信和无线电信号可以降低。来自GPS卫星的信号可用于表征电离层闪烁的位置和程度,并改善预测电离层闪烁的模型。地球磁场最弱的南大西洋中的地区,被称为南大西洋磁异常(SAMA),可能是电离层闪烁由于来自地球辐射带的高能粒子的沉淀而更严重的区域。本文介绍了通过2007年南半球中南半球中的和极光纬度的专用闪烁监测器接收的GPS信号观察到的一些第一电离层闪烁。

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