3D TOMOGRAPHY OF IONOSPHERIC ANOMALIES AFTER THE 2020 TURKEY EARTHQUAKE AND TSUNAMI USING GNSS-TEC

Global Navigation Satellite System (GNSS) satellite observations can obtain Total Electron Content (TEC) values in the ionosphere layer. The TEC value is obtained by decreasing the phase difference of the GNSS satellite’s two carrier waves (L-band). The calculation of the TEC value using GNSS can be...

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Autores principales: Mokhamad Nur Cahyadi *email correspondence: cahyadi@geodesy.its.ac.id, Ira Mutiara Anjasmara, Ihsan Naufal Muafiry, Nurrohmat Widjajanti, Deasy Arisa, Buldan Muslim, Meilfan Eka Putra
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Publicado: Tsunami Society International 2021
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Acceso en línea:https://doaj.org/article/6babfaaf3a9745f994886751f2da4e75
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spelling oai:doaj.org-article:6babfaaf3a9745f994886751f2da4e752021-11-07T23:06:40Z3D TOMOGRAPHY OF IONOSPHERIC ANOMALIES AFTER THE 2020 TURKEY EARTHQUAKE AND TSUNAMI USING GNSS-TEC8755-6839https://doaj.org/article/6babfaaf3a9745f994886751f2da4e752021-10-01T00:00:00Zhttp://www.tsunamisociety.org/403CahyadiEtAl.pdfhttps://doaj.org/toc/8755-6839Global Navigation Satellite System (GNSS) satellite observations can obtain Total Electron Content (TEC) values in the ionosphere layer. The TEC value is obtained by decreasing the phase difference of the GNSS satellite’s two carrier waves (L-band). The calculation of the TEC value using GNSS can be used in disaster phenomena such as earthquakes observed in this study. The earthquake phenomenon can cause vertical deformation in the Earth’s crust, resulting in the appearance of acoustic waves propagating towards the ionosphere layer and changes in the ionosphere density in a moment. A propagating gravity wave has a speed of 0.3 km/ s towards the ionosphere layer. This disturbed ionosphere layer was detected within minutes of the mainshock. The anomaly in this study was detected by Global Positioning System (GPS) Pseudo Random Noise (PRN) 16 from 16 observation GNSS stations on the mainland of Turkey. The observed ionosphere anomalies were then modeled using tomography modelling to obtain spatial information from these anomalies. The tomography results found that the PRN 16 GPS satellites contained positive and negative anomalies located northeast of the epicenter.Mokhamad Nur Cahyadi *email correspondence: cahyadi@geodesy.its.ac.idIra Mutiara AnjasmaraIhsan Naufal MuafiryNurrohmat WidjajantiDeasy ArisaBuldan MuslimMeilfan Eka PutraTsunami Society Internationalarticle3d tomographyearthquakegnsstotal electron contentturkey earthquakeOceanographyGC1-1581ENScience of Tsunami Hazards, Vol 40, Iss 3, Pp 166-177 (2021)
institution DOAJ
collection DOAJ
language EN
topic 3d tomography
earthquake
gnss
total electron content
turkey earthquake
Oceanography
GC1-1581
spellingShingle 3d tomography
earthquake
gnss
total electron content
turkey earthquake
Oceanography
GC1-1581
Mokhamad Nur Cahyadi *email correspondence: cahyadi@geodesy.its.ac.id
Ira Mutiara Anjasmara
Ihsan Naufal Muafiry
Nurrohmat Widjajanti
Deasy Arisa
Buldan Muslim
Meilfan Eka Putra
3D TOMOGRAPHY OF IONOSPHERIC ANOMALIES AFTER THE 2020 TURKEY EARTHQUAKE AND TSUNAMI USING GNSS-TEC
description Global Navigation Satellite System (GNSS) satellite observations can obtain Total Electron Content (TEC) values in the ionosphere layer. The TEC value is obtained by decreasing the phase difference of the GNSS satellite’s two carrier waves (L-band). The calculation of the TEC value using GNSS can be used in disaster phenomena such as earthquakes observed in this study. The earthquake phenomenon can cause vertical deformation in the Earth’s crust, resulting in the appearance of acoustic waves propagating towards the ionosphere layer and changes in the ionosphere density in a moment. A propagating gravity wave has a speed of 0.3 km/ s towards the ionosphere layer. This disturbed ionosphere layer was detected within minutes of the mainshock. The anomaly in this study was detected by Global Positioning System (GPS) Pseudo Random Noise (PRN) 16 from 16 observation GNSS stations on the mainland of Turkey. The observed ionosphere anomalies were then modeled using tomography modelling to obtain spatial information from these anomalies. The tomography results found that the PRN 16 GPS satellites contained positive and negative anomalies located northeast of the epicenter.
format article
author Mokhamad Nur Cahyadi *email correspondence: cahyadi@geodesy.its.ac.id
Ira Mutiara Anjasmara
Ihsan Naufal Muafiry
Nurrohmat Widjajanti
Deasy Arisa
Buldan Muslim
Meilfan Eka Putra
author_facet Mokhamad Nur Cahyadi *email correspondence: cahyadi@geodesy.its.ac.id
Ira Mutiara Anjasmara
Ihsan Naufal Muafiry
Nurrohmat Widjajanti
Deasy Arisa
Buldan Muslim
Meilfan Eka Putra
author_sort Mokhamad Nur Cahyadi *email correspondence: cahyadi@geodesy.its.ac.id
title 3D TOMOGRAPHY OF IONOSPHERIC ANOMALIES AFTER THE 2020 TURKEY EARTHQUAKE AND TSUNAMI USING GNSS-TEC
title_short 3D TOMOGRAPHY OF IONOSPHERIC ANOMALIES AFTER THE 2020 TURKEY EARTHQUAKE AND TSUNAMI USING GNSS-TEC
title_full 3D TOMOGRAPHY OF IONOSPHERIC ANOMALIES AFTER THE 2020 TURKEY EARTHQUAKE AND TSUNAMI USING GNSS-TEC
title_fullStr 3D TOMOGRAPHY OF IONOSPHERIC ANOMALIES AFTER THE 2020 TURKEY EARTHQUAKE AND TSUNAMI USING GNSS-TEC
title_full_unstemmed 3D TOMOGRAPHY OF IONOSPHERIC ANOMALIES AFTER THE 2020 TURKEY EARTHQUAKE AND TSUNAMI USING GNSS-TEC
title_sort 3d tomography of ionospheric anomalies after the 2020 turkey earthquake and tsunami using gnss-tec
publisher Tsunami Society International
publishDate 2021
url https://doaj.org/article/6babfaaf3a9745f994886751f2da4e75
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