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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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 |
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15 |
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19 |
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4879 |
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1782336084914470912 |