新西兰三个Mw>6.5 EQ的电离层和大气异常调查

IF 2.1 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
Muhammad Arqim Adil , Ayesha Abbas , Muhsan Ehsan , Munawar Shah , Najam Abbas Naqvi , Amjad Alie
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引用次数: 12

摘要

双频全球定位系统(GPS)提供了探测地震或地磁风暴效应引起的总电子含量(TEC)变化的电离层扰动的见解。在本文中,我们研究了三个大震级(Mw>;6.5)和浅震源深度<;从震中周围的国际GNSS服务(IGS)站检索到的每日GPS TEC时间序列中,新西兰的20公里EQ。此外,在活跃风暴日发生两次EQ(Mw 7.8和Mw 6.8)和一次EQ 6.6(以下简称地磁暴EQ事件)之前的5-15天内,地磁活动完全平静。异常是基于运行中值和四分位数区间(IQR)的统计分析来检测的,以表示每个EQ之前30天和之后10天的每日TEC时间序列中的异常;在Mw 7.8和Mw 6.8的两个EQ之前的5–15天内,UT=15–24小时(对于新西兰,UT=LT+13)期间的2个TECU。然而,由于活跃的风暴条件(Kp>;3;Dst<;−50 nT),地磁风暴EQ事件(Mw 6.6)在主震前后远远超过5–15天,产生了一系列正负异常。此外,地磁风暴异常在Mw 6.6 EQ日活跃风暴条件下占主导地位。为了验证电离层异常可能是地震前兆,还检查了相对湿度和OLR(输出长波辐射)的大气异常,以显示电离层异常从岩石圈经由大气向电离层的演变。此外,由于地磁暴EQ的性质,在Mw 7.8和Mw 6.8震中上EQ引起的规则和并置大气异常以及在Mw 6.6发震带上存在不规则大气异常。在未来EQ震中的地震准备阶段,观测到的EQ异常将有助于改进岩石圈-大气-电离层耦合假说。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Investigation of ionospheric and atmospheric anomalies associated with three Mw >6.5 EQs in New Zealand

The dual-frequency Global Positioning System (GPS) provides insights to detect the ionospheric perturbations with Total Electron Content (TEC) variations induced by the Earthquakes (EQs) or geomagnetic storm effects. In this paper, we investigate abnormal ionospheric signatures before three large magnitudes (Mw > 6.5) and shallow hypocentral depth < 20 km EQs in New Zealand from daily GPS TEC time series retrieved from International GNSS Services (IGS) stations around the epicenter. Furthermore, geomagnetic activities are completely quiet within 5–15 days before two EQs (Mw 7.8 and Mw 6.8) and one EQ of Mw 6.6 occurred in active storm days (hereafter, geomagnetic storm-EQ event). The anomalies are detected on the basis of a statistical analysis of running median and Inter Quartile Range (IQR) to signify the abnormality in daily TEC time series for 30 days before and 10 days after each EQ. We observe less intensity TEC anomalies of < 2 TECU during UT = 15–24 h (for New Zealand, UT = LT + 13) within 5–15 days before two EQs of Mw 7.8 and Mw 6.8. Whereas, a chain of positive and negative anomalies is generated by geomagnetic storm-EQ event (Mw 6.6) far beyond 5–15 days before and after the main shock due to active storm conditions (Kp> 3; Dst < −50 nT). Furthermore, geomagnetic storm anomalies are dominant on Mw 6.6 EQ day to active storm conditions. To validate the ionospheric anomalies as possible seismic precursors, the atmospheric anomalies in relative humidity and OLR (outgoing longwave radiations) are also examined to exhibit the evolution of ionospheric anomalies from the lithosphere to ionosphere via the atmosphere. Moreover, EQ induced regular and collocated atmospheric anomalies over the epicenters of Mw 7.8 and Mw 6.8 and irregular atmospheric anomalies exist over the seismogenic zone of Mw 6.6 due to geomagnetic storm-EQ nature. The observed EQ anomalies will aid in the improvement of lithosphere atmosphere ionosphere coupling hypothesis during the seismic preparation phase over the epicenter of future EQ.

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来源期刊
Journal of Geodynamics
Journal of Geodynamics 地学-地球化学与地球物理
CiteScore
4.60
自引率
0.00%
发文量
21
审稿时长
6-12 weeks
期刊介绍: The Journal of Geodynamics is an international and interdisciplinary forum for the publication of results and discussions of solid earth research in geodetic, geophysical, geological and geochemical geodynamics, with special emphasis on the large scale processes involved.
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