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Ionospheric monitoring by the Global Navigation Satellite System (GNSS).

机译:全球导航卫星系统(GNSS)对电离层的监测。

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摘要

The ionosphere reacts to geophysical events, such as earthquakes, tsunamis, surface explosions, underground nuclear explosions (UNE), etc. The Global Navigation Satellite System (GNSS) remote sensing (RS) enables monitoring of the ionospheric disturbances excited by these events. The purpose of this dissertation is to use GNSS RS to detect, discriminate, model and monitor ionospheric disturbances induced by earthquakes and UNEs.;Ionospheric delay, which can be derived from dual frequency GNSS signals, is converted to the total electron contents (TEC) along the signal path. After eliminating the main trend of TEC by taking the numerical third order horizontal 3-point derivatives, the traveling ionospheric disturbances (TIDs) are isolated. Since a TID can be generated due to various events, the source of TID must be verified. In this dissertation, the characteristics of the TID waves induced by an earthquake and an UNE are examined. The case studies are: (1) M9.0 2011 Tohoku, Japan earthquake, (2) 2006 North Korean UNE, and (3) 2009 North Korean UNE. From these experiments, the TIDs resulting from different types of events were characterized and discriminated due to the different waveform properties.;In addition, the epicenter of the point source can be determined by TID observations. In experiment (2), the 2009 North Korean UNE was examined, using data from eleven nearby GNSS stations. Within a few hours from the explosion, the GNSS stations detected the TIDs, whose arrival time for each station formulated the linear model with respect to the distance to the station. TIDs were observed to propagate with speeds of roughly 150 - 400 m/s at stations about 365 km to 1330 km from the explosion site. Considering the wind effect, the wind-adjusted TIDs located the UNE to within about 2.7 km of its seismically determined epicenter.;Through the case studies, the distinctive signatures of different events were demonstrated, which suggests the uniqueness of TIDs excited by different types of events. The major contributions of this dissertation is a demonstration of the applicability of GNSS RS to detect and discriminate geophysical events causing TIDs, and its ability to determine the epicenter of the point source.
机译:电离层对诸如地震,海啸,地表爆炸,地下核爆炸(UNE)等地球物理事件做出反应。全球导航卫星系统(GNSS)遥感(RS)能够监视由这些事件引起的电离层扰动。本文的目的是利用GNSS RS对地震和UNE引起的电离层扰动进行检测,判别,建模和监测。可将来自双频GNSS信号的电离层延迟转换为总电子含量(TEC)沿着信号路径。通过采用数值三阶水平三点导数消除了TEC的主要趋势之后,隔离了行进的电离层扰动(TID)。由于可以由于各种事件而生成TID,因此必须验证TID的来源。本文研究了地震和UNE引起的TID波的特征。案例研究包括:(1)2011年日本东北东北部M9.0级地震;(2)2006年朝鲜UNE,以及(3)2009年朝鲜UNE。从这些实验中,由于波形特性不同,对由不同类型事件产生的TID进行了表征和区分。此外,可以通过TID观测确定点源的震中。在实验(2)中,使用来自附近11个GNSS站的数据对2009年朝鲜UNE进行了检查。爆炸发生后的几个小时内,GNSS台站检测到了TID,每个台站的到达时间都针对到台站的距离制定了线性模型。在离爆炸地点约365 km至1330 km处,观察到的TID以大约150-400 m / s的速度传播。考虑到风的影响,经风调节的TID将UNE定位在其地震确定的震中约2.7 km之内。通过案例研究,展示了不同事件的独特特征,这表明由不同类型的TID激发的TID的独特性事件。本论文的主要贡献是证明了GNSS RS在探测和识别引起TID的地球物理事件方面的适用性,以及确定点源震中的能力。

著录项

  • 作者

    Park, Jihye.;

  • 作者单位

    The Ohio State University.;

  • 授予单位 The Ohio State University.;
  • 学科 Geodesy.;Engineering Geological.;Engineering Geophysical.;Remote Sensing.
  • 学位 Ph.D.
  • 年度 2012
  • 页码 203 p.
  • 总页数 203
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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