Analysis of Ionospheric Anomalies before the Tonga Volcanic Eruption on 15 January 2022

In this paper, GNSS stations’ observational data, global ionospheric maps (GIM) and the electron density of FORMOSAT-7/COSMIC-2 occultation are used to study ionospheric anomalies before the submarine volcanic eruption of Hunga Tonga–Hunga Ha’apai on 15 January 2022. (i) We detect the negative total...

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Published in:Remote Sensing
Main Authors: Jiandi Feng, Yunbin Yuan, Ting Zhang, Zhihao Zhang, Di Meng
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2023
Subjects:
EIA
Q
Eia
Online Access:https://doi.org/10.3390/rs15194879
https://doaj.org/article/2ee3fb4468e14e95937ff2e6ed1dfaf1
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spelling ftdoajarticles:oai:doaj.org/article:2ee3fb4468e14e95937ff2e6ed1dfaf1 2023-11-12T04:03:05+01:00 Analysis of Ionospheric Anomalies before the Tonga Volcanic Eruption on 15 January 2022 Jiandi Feng Yunbin Yuan Ting Zhang Zhihao Zhang Di Meng 2023-10-01T00:00:00Z https://doi.org/10.3390/rs15194879 https://doaj.org/article/2ee3fb4468e14e95937ff2e6ed1dfaf1 EN eng MDPI AG https://www.mdpi.com/2072-4292/15/19/4879 https://doaj.org/toc/2072-4292 doi:10.3390/rs15194879 2072-4292 https://doaj.org/article/2ee3fb4468e14e95937ff2e6ed1dfaf1 Remote Sensing, Vol 15, Iss 4879, p 4879 (2023) Tonga volcanic eruption ionospheric anomaly anomaly detection method EIA Science Q article 2023 ftdoajarticles https://doi.org/10.3390/rs15194879 2023-10-15T00:35:17Z In this paper, GNSS stations’ observational data, global ionospheric maps (GIM) and the electron density of FORMOSAT-7/COSMIC-2 occultation are used to study ionospheric anomalies before the submarine volcanic eruption of Hunga Tonga–Hunga Ha’apai on 15 January 2022. (i) We detect the negative total electron content (TEC) anomalies by three GNSS stations on 5 January before the volcanic eruption after excluding the influence of solar and geomagnetic disturbances and lower atmospheric forcing. The GIMs also detect the negative anomaly in the global ionospheric TEC only near the epicenter of the eruption on 5 January, with a maximum outlier exceeding 6 TECU. (ii) From 1 to 3 January (local time), the equatorial ionization anomaly (EIA) peak shifts significantly towards the Antarctic from afternoon to night. The equatorial ionization anomaly double peak decreases from 4 January, and the EIA double peak disappears and merges into a single peak on 7 January. Meanwhile, the diurnal maxima of TEC at TONG station decrease by nearly 10 TECU and only one diurnal maximum occurred on 4 January (i.e., 5 January of UT), but the significant ionospheric diurnal double-maxima (DDM) are observed on other dates. (iii) We find a maximum value exceeding NmF2 at an altitude of 100~130 km above the volcanic eruption on 5 January (i.e., a sporadic E layer), with an electron density of 7.5 × 10 5 el/cm 3 . Article in Journal/Newspaper Antarc* Antarctic Directory of Open Access Journals: DOAJ Articles Antarctic Eia ENVELOPE(7.755,7.755,63.024,63.024) The Antarctic Tonga ENVELOPE(7.990,7.990,63.065,63.065) Remote Sensing 15 19 4879
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Tonga volcanic eruption
ionospheric anomaly
anomaly detection method
EIA
Science
Q
spellingShingle Tonga volcanic eruption
ionospheric anomaly
anomaly detection method
EIA
Science
Q
Jiandi Feng
Yunbin Yuan
Ting Zhang
Zhihao Zhang
Di Meng
Analysis of Ionospheric Anomalies before the Tonga Volcanic Eruption on 15 January 2022
topic_facet Tonga volcanic eruption
ionospheric anomaly
anomaly detection method
EIA
Science
Q
description In this paper, GNSS stations’ observational data, global ionospheric maps (GIM) and the electron density of FORMOSAT-7/COSMIC-2 occultation are used to study ionospheric anomalies before the submarine volcanic eruption of Hunga Tonga–Hunga Ha’apai on 15 January 2022. (i) We detect the negative total electron content (TEC) anomalies by three GNSS stations on 5 January before the volcanic eruption after excluding the influence of solar and geomagnetic disturbances and lower atmospheric forcing. The GIMs also detect the negative anomaly in the global ionospheric TEC only near the epicenter of the eruption on 5 January, with a maximum outlier exceeding 6 TECU. (ii) From 1 to 3 January (local time), the equatorial ionization anomaly (EIA) peak shifts significantly towards the Antarctic from afternoon to night. The equatorial ionization anomaly double peak decreases from 4 January, and the EIA double peak disappears and merges into a single peak on 7 January. Meanwhile, the diurnal maxima of TEC at TONG station decrease by nearly 10 TECU and only one diurnal maximum occurred on 4 January (i.e., 5 January of UT), but the significant ionospheric diurnal double-maxima (DDM) are observed on other dates. (iii) We find a maximum value exceeding NmF2 at an altitude of 100~130 km above the volcanic eruption on 5 January (i.e., a sporadic E layer), with an electron density of 7.5 × 10 5 el/cm 3 .
format Article in Journal/Newspaper
author Jiandi Feng
Yunbin Yuan
Ting Zhang
Zhihao Zhang
Di Meng
author_facet Jiandi Feng
Yunbin Yuan
Ting Zhang
Zhihao Zhang
Di Meng
author_sort Jiandi Feng
title Analysis of Ionospheric Anomalies before the Tonga Volcanic Eruption on 15 January 2022
title_short Analysis of Ionospheric Anomalies before the Tonga Volcanic Eruption on 15 January 2022
title_full Analysis of Ionospheric Anomalies before the Tonga Volcanic Eruption on 15 January 2022
title_fullStr Analysis of Ionospheric Anomalies before the Tonga Volcanic Eruption on 15 January 2022
title_full_unstemmed Analysis of Ionospheric Anomalies before the Tonga Volcanic Eruption on 15 January 2022
title_sort analysis of ionospheric anomalies before the tonga volcanic eruption on 15 january 2022
publisher MDPI AG
publishDate 2023
url https://doi.org/10.3390/rs15194879
https://doaj.org/article/2ee3fb4468e14e95937ff2e6ed1dfaf1
long_lat ENVELOPE(7.755,7.755,63.024,63.024)
ENVELOPE(7.990,7.990,63.065,63.065)
geographic Antarctic
Eia
The Antarctic
Tonga
geographic_facet Antarctic
Eia
The Antarctic
Tonga
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_source Remote Sensing, Vol 15, Iss 4879, p 4879 (2023)
op_relation https://www.mdpi.com/2072-4292/15/19/4879
https://doaj.org/toc/2072-4292
doi:10.3390/rs15194879
2072-4292
https://doaj.org/article/2ee3fb4468e14e95937ff2e6ed1dfaf1
op_doi https://doi.org/10.3390/rs15194879
container_title Remote Sensing
container_volume 15
container_issue 19
container_start_page 4879
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