Analysis of Ionospheric Disturbances Caused by the 2018 Bering Sea Meteor Explosion Based on GPS Observations

The Bering Sea meteor explosion that occurred on 18 December 2018 provides a good opportunity to study the ionospheric disturbances caused by meteor explosions. Total electron content (TEC) is the core parameter of ionospheric analysis. TEC and its changes can be accurately estimated based on the Gl...

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Published in:Sensors
Main Authors: Yiyong Luo, Yibin Yao, Lulu Shan
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2020
Subjects:
TEC
TID
Online Access:https://doi.org/10.3390/s20113201
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spelling ftmdpi:oai:mdpi.com:/1424-8220/20/11/3201/ 2023-08-20T04:05:36+02:00 Analysis of Ionospheric Disturbances Caused by the 2018 Bering Sea Meteor Explosion Based on GPS Observations Yiyong Luo Yibin Yao Lulu Shan 2020-06-04 application/pdf https://doi.org/10.3390/s20113201 EN eng Multidisciplinary Digital Publishing Institute Remote Sensors https://dx.doi.org/10.3390/s20113201 https://creativecommons.org/licenses/by/4.0/ Sensors; Volume 20; Issue 11; Pages: 3201 meteor explosion TEC TID characteristics of TID Text 2020 ftmdpi https://doi.org/10.3390/s20113201 2023-07-31T23:35:49Z The Bering Sea meteor explosion that occurred on 18 December 2018 provides a good opportunity to study the ionospheric disturbances caused by meteor explosions. Total electron content (TEC) is the core parameter of ionospheric analysis. TEC and its changes can be accurately estimated based on the Global Positioning System (GPS). TID is detected in time and frequency domain based on power spectrum and Butterworth filtering method. By analyzing the waveform, period, wavelength, propagation speed and space-time distribution of TID, the location of the TID source is determined, and the process of TID formation and propagation is understood. The TID caused by meteor explosions has significant anisotropy characteristic. Two types of TID were found. For the first type, the average horizontal propagation velocity is 250.22 ± 5.98 m/s, the wavelength is ~135–240 km, the average period is about 12 min, and the propagation distance is less than 1400 km. About 8 min after the meteor explosion, the first type of TID source formed and propagated radially at the velocity of 250.22 ± 5.98 m/s. For the second type, the propagation velocity is ~434.02 m/s. According to the waveform, period, wavelength and propagation velocity of the TID, it is diagnosed to be the midscale traveling ionospheric disturbances (MSTID). Based on the characteristics of TID, we infer that the TID is excited by the gravity waves generated by the meteor explosion, which is in accordance with the propagation law of gravity waves in the ionosphere. And it is estimated that the average velocity of the up-going gravity waves is about 464.58 m/s. A simple model was established to explain the formation and the propagation of this TID, and to verify the characteristics of the TID propagation caused by nuclear explosion, earthquake, tsunami, and Chelyabinsk meteorite blast. It is estimated that the position of the TID source is consistent with the meteor explosion point, which further indicates that the TID is caused by the meteor explosion and propagates ... Text Bering Sea MDPI Open Access Publishing Bering Sea Butterworth ENVELOPE(66.733,66.733,-70.700,-70.700) Sensors 20 11 3201
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic meteor explosion
TEC
TID
characteristics of TID
spellingShingle meteor explosion
TEC
TID
characteristics of TID
Yiyong Luo
Yibin Yao
Lulu Shan
Analysis of Ionospheric Disturbances Caused by the 2018 Bering Sea Meteor Explosion Based on GPS Observations
topic_facet meteor explosion
TEC
TID
characteristics of TID
description The Bering Sea meteor explosion that occurred on 18 December 2018 provides a good opportunity to study the ionospheric disturbances caused by meteor explosions. Total electron content (TEC) is the core parameter of ionospheric analysis. TEC and its changes can be accurately estimated based on the Global Positioning System (GPS). TID is detected in time and frequency domain based on power spectrum and Butterworth filtering method. By analyzing the waveform, period, wavelength, propagation speed and space-time distribution of TID, the location of the TID source is determined, and the process of TID formation and propagation is understood. The TID caused by meteor explosions has significant anisotropy characteristic. Two types of TID were found. For the first type, the average horizontal propagation velocity is 250.22 ± 5.98 m/s, the wavelength is ~135–240 km, the average period is about 12 min, and the propagation distance is less than 1400 km. About 8 min after the meteor explosion, the first type of TID source formed and propagated radially at the velocity of 250.22 ± 5.98 m/s. For the second type, the propagation velocity is ~434.02 m/s. According to the waveform, period, wavelength and propagation velocity of the TID, it is diagnosed to be the midscale traveling ionospheric disturbances (MSTID). Based on the characteristics of TID, we infer that the TID is excited by the gravity waves generated by the meteor explosion, which is in accordance with the propagation law of gravity waves in the ionosphere. And it is estimated that the average velocity of the up-going gravity waves is about 464.58 m/s. A simple model was established to explain the formation and the propagation of this TID, and to verify the characteristics of the TID propagation caused by nuclear explosion, earthquake, tsunami, and Chelyabinsk meteorite blast. It is estimated that the position of the TID source is consistent with the meteor explosion point, which further indicates that the TID is caused by the meteor explosion and propagates ...
format Text
author Yiyong Luo
Yibin Yao
Lulu Shan
author_facet Yiyong Luo
Yibin Yao
Lulu Shan
author_sort Yiyong Luo
title Analysis of Ionospheric Disturbances Caused by the 2018 Bering Sea Meteor Explosion Based on GPS Observations
title_short Analysis of Ionospheric Disturbances Caused by the 2018 Bering Sea Meteor Explosion Based on GPS Observations
title_full Analysis of Ionospheric Disturbances Caused by the 2018 Bering Sea Meteor Explosion Based on GPS Observations
title_fullStr Analysis of Ionospheric Disturbances Caused by the 2018 Bering Sea Meteor Explosion Based on GPS Observations
title_full_unstemmed Analysis of Ionospheric Disturbances Caused by the 2018 Bering Sea Meteor Explosion Based on GPS Observations
title_sort analysis of ionospheric disturbances caused by the 2018 bering sea meteor explosion based on gps observations
publisher Multidisciplinary Digital Publishing Institute
publishDate 2020
url https://doi.org/10.3390/s20113201
long_lat ENVELOPE(66.733,66.733,-70.700,-70.700)
geographic Bering Sea
Butterworth
geographic_facet Bering Sea
Butterworth
genre Bering Sea
genre_facet Bering Sea
op_source Sensors; Volume 20; Issue 11; Pages: 3201
op_relation Remote Sensors
https://dx.doi.org/10.3390/s20113201
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/s20113201
container_title Sensors
container_volume 20
container_issue 11
container_start_page 3201
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