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近实时确定同震行进电离层扰动(CTID)的时空特征。

Determining spatio-temporal characteristics of coseismic travelling ionospheric disturbances (CTID) in near real-time.

作者信息

Maletckii Boris, Astafyeva Elvira

机构信息

CNRS UMR 7154, Institut de Physique du Globe de Paris (IPGP), Université de Paris, 35-39 Rue Hélène Brion, 75013, Paris, France.

出版信息

Sci Rep. 2021 Oct 21;11(1):20783. doi: 10.1038/s41598-021-99906-5.

Abstract

Earthquakes are known to generate ionospheric disturbances that are commonly referred to as co-seismic travelling ionospheric disturbances (CTID). In this work, for the first time, we present a novel method that enables to automatically detect CTID in ionospheric GNSS-data, and to determine their spatio-temporal characteristics (velocity and azimuth of propagation) in near-real time (NRT), i.e., less than 15 min after an earthquake. The obtained instantaneous velocities allow us to understand the evolution of CTID and to estimate the location of the CTID source in NRT. Furthermore, also for the first time, we developed a concept of real-time travel-time diagrams that aid to verify the correlation with the source and to estimate additionally the propagation speed of the observed CTID. We apply our methods to the Mw7.4 Sanriku earthquake of 09/03/2011 and the Mw9.0 Tohoku earthquake of 11/03/2011, and we make a NRT analysis of the dynamics of CTID driven by these seismic events. We show that the best results are achieved with high-rate 1 Hz data. While the first tests are made on CTID, our method is also applicable for detection and determining of spatio-temporal characteristics of other travelling ionospheric disturbances that often occur in the ionosphere driven by many geophysical phenomena.

摘要

众所周知,地震会产生电离层扰动,通常被称为同震行进电离层扰动(CTID)。在这项工作中,我们首次提出了一种新颖的方法,该方法能够自动检测电离层全球导航卫星系统(GNSS)数据中的CTID,并近实时(NRT)(即地震发生后不到15分钟)确定其时空特征(传播速度和方位角)。所获得的瞬时速度使我们能够了解CTID的演变,并在近实时估计CTID源的位置。此外,我们还首次开发了实时走时图的概念,这有助于验证与源的相关性,并额外估计观测到的CTID的传播速度。我们将我们的方法应用于2011年3月9日Mw7.4的三陆地震和2011年3月11日Mw9.0的东北地震,并对由这些地震事件驱动的CTID的动力学进行了近实时分析。我们表明,使用1Hz的高速率数据可获得最佳结果。虽然首次测试是针对CTID进行的,但我们的方法也适用于检测和确定由许多地球物理现象驱动的电离层中经常出现的其他行进电离层扰动的时空特征。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ef87/8531289/d61893e724d5/41598_2021_99906_Fig1_HTML.jpg

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