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首页> 外文期刊>Scientific reports. >Real-Time Detection of Tsunami Ionospheric Disturbances with a Stand-Alone GNSS Receiver: A Preliminary Feasibility Demonstration
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Real-Time Detection of Tsunami Ionospheric Disturbances with a Stand-Alone GNSS Receiver: A Preliminary Feasibility Demonstration

机译:用独立GNSS接收器实时检测海啸电离层干扰:初步可行性示范

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It is well known that tsunamis can produce gravity waves that propagate up to the ionosphere generating disturbed electron densities in the E and F regions. These ionospheric disturbances can be studied in detail using ionospheric total electron content (TEC) measurements collected by continuously operating ground-based receivers from the Global Navigation Satellite Systems (GNSS). Here, we present results using a new approach, named VARION (Variometric Approach for Real-Time Ionosphere Observation), and estimate slant TEC (sTEC) variations in a real-time scenario. Using the VARION algorithm we compute TEC variations at 56 GPS receivers in Hawaii as induced by the 2012 Haida Gwaii tsunami event. We observe TEC perturbations with amplitudes of up to 0.25 TEC units and traveling ionospheric perturbations (TIDs) moving away from the earthquake epicenter at an approximate speed of 316 m/s. We perform a wavelet analysis to analyze localized variations of power in the TEC time series and we find perturbation periods consistent with a tsunami typical deep ocean period. Finally, we present comparisons with the real-time tsunami MOST (Method of Splitting Tsunami) model produced by the NOAA Center for Tsunami Research and we observe variations in TEC that correlate in time and space with the tsunami waves.
机译:众所周知,海啸可以产生重力波,该重力波向E和F区域中的电离层产生干扰的电子密度。可以使用通过从全球导航卫星系统(GNSS)的连续操作地基接收器收集的电离层总电子含量(TEC)测量来详细研究这些电离层干扰。在这里,我们使用新方法的结果,命名变量(用于实时电离层观察的尺寸方法),并在实时方案中估计倾斜TEC(STEC)变化。使用变量算法,我们在2012年海达Gwaii海啸事件引发的夏威夷56个GPS接收器中计算TEC变化。我们观察到具有高达0.25tEC单元的幅度的TEC扰动,并以316米/秒的近似速度远离地震震中的电离层扰动(TID)。我们执行小波分析,分析TEC时间序列中的局部电力变化,我们发现与海啸典型深海时期一致的扰动期。最后,我们对Noaa Centres生产的实时海啸进行了比较(分裂海啸方法)模型,用于海啸研究,观察TEC的变化与海啸波的时间和空间相关。

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