首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >Tomographic Imaging of Traveling Ionospheric Disturbances Using GNSS and Geostationary Satellite Observations
【24h】

Tomographic Imaging of Traveling Ionospheric Disturbances Using GNSS and Geostationary Satellite Observations

机译:层析成像的电离层干扰使用GNSS和同步卫星观测

获取原文
获取原文并翻译 | 示例
           

摘要

Traveling ionospheric disturbances (TIDs) are the manifestations of atmospheric gravity waves in the ionosphere. These disturbances have practical importance because they affect satellite navigation technologies such as Global Navigational Satellite System (GNSS), causing degradation in precise positioning applications. They also have scientific significance as their generation mechanisms and propagation are not fully understood. While there are specific instruments that can measure TIDs in certain locations, there is a need for wide-area observations across extended geographical regions to continuously monitor their onset and spatial and temporal characteristics. This paper evaluates the use of observations from ground-based geodetic GNSS receivers to image TIDs using ionospheric tomography and data assimilation. Certain GNSS receivers also monitor signals from geostationary (GEO) satellites, which provide a unique perspective on the TID. The advantage of using the GEO data is investigated. A computerized simulation of GNSS observations is used for evaluation of the Multi-Instrument Data Analysis System (MIDAS) with GEO and regular GNSS geometry. The simulated observations are generated by integrating the electron density through a modeled TID-perturbed dynamic ionosphere between actual receiver and satellite positions. The output 3-D electron density image series generated from the synthetic data by the MIDAS ionospheric tomography and data assimilation algorithm are compared with the input model ionosphere. Results show that GEO geometry improves the reconstruction of medium-scale TIDs (MSTIDs) and smaller LSTIDs in cases where the movement of regular GNSS satellites in Medium Earth orbit (MEO) may otherwise introduce distortions to the observations.
机译:电离层扰动(tid)旅行大气重力波的表现电离层。因为他们影响卫星重要性如全球导航技术导航卫星系统(GNSS),导致在精确定位应用程序中退化。他们也有科学意义的生成机制和传播完全理解。工具,可以测量tid在某些的位置,有一个广域的必要性观察跨地理区域扩展持续监测他们的发病和空间和时间特性。评估使用的观测地面大地GNSS接收器的形象tid用电离层断层扫描和数据同化。从地球静止轨道(GEO)卫星信号,TID提供独特的视角。使用地理数据的优势调查。观察用于评估Multi-Instrument数据分析系统(麦得斯)GEO和常规GNSS几何。观察是由整合生成的通过建模TID-perturbed电子密度动态实际接收机和之间的电离层卫星的位置。密度图像合成产生的系列MIDAS电离层数据的断层扫描和数据同化算法相比输入模型电离层。几何提高了重建中等规模的tid (MSTIDs)和小LSTIDs定期的运动GNSS的情况卫星介质地球轨道(MEO)否则扭曲介绍观察。

著录项

相似文献

  • 外文文献
  • 中文文献
获取原文

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