首页> 美国卫生研究院文献>Scientific Reports >Real-Time Detection of Tsunami Ionospheric Disturbances with a Stand-Alone GNSS Receiver: A Preliminary Feasibility Demonstration
【2h】

Real-Time Detection of Tsunami Ionospheric Disturbances with a Stand-Alone GNSS Receiver: A Preliminary Feasibility Demonstration

机译:使用独立的GNSS接收器实时检测海啸电离层扰动:初步可行性论证

代理获取
本网站仅为用户提供外文OA文献查询和代理获取服务,本网站没有原文。下单后我们将采用程序或人工为您竭诚获取高质量的原文,但由于OA文献来源多样且变更频繁,仍可能出现获取不到、文献不完整或与标题不符等情况,如果获取不到我们将提供退款服务。请知悉。

摘要

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,海啸会产生引力波,这些引力波会传播到电离层,从而在E和F区域产生扰动的电子密度。可以使用电离层总电子含量(TEC)测量值对这些电离层扰动进行详细研究,这些测量值是由来自全球导航卫星系统(GNSS)的连续运行的地面接收器收集的。在这里,我们使用名为VARION(用于实时电离层观测的可变方法)的新方法介绍结果,并在实时场景中估算倾斜TEC(sTEC)的变化。使用VARION算法,我们可以计算出2012年海达瓜(Haida Gwaii)海啸事件引起的夏威夷56个GPS接收器的TEC变化。我们观察到TEC扰动的振幅高达0.25 TEC单位,而行进的电离层扰动(TID)以大约316 m / s的速度从地震震中移开。我们执行小波分析来分析TEC时间序列中的局部功率变化,我们发现与海啸典型的深海时期一致的扰动时期。最后,我们将与NOAA海啸研究中心制作的实时海啸MOST(分裂海啸的方法)模型进行比较,并观察TEC的变化,该变化在时间和空间上与海啸相关。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
代理获取

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号