dc.contributor.author | Aa, Ercha | |
dc.contributor.author | Zhang, Shun-Rong | |
dc.contributor.author | Wang, Wenbing | |
dc.contributor.author | Erickson, Philip J. | |
dc.contributor.author | Qian, Liying | |
dc.contributor.author | Eastes, Richard W. | |
dc.contributor.author | Harding, Brian | |
dc.contributor.author | Immel, Thomas | |
dc.contributor.author | Karan, Deepak | |
dc.contributor.author | Daniell, Robert E. | |
dc.contributor.author | Coster, Anthea J. | |
dc.contributor.author | Goncharenko, Larisa P. | |
dc.contributor.author | Vierinen, Juha | |
dc.contributor.author | Cai, Xuguang | |
dc.contributor.author | Spicher, Andres | |
dc.date.accessioned | 2022-11-29T08:32:34Z | |
dc.date.available | 2022-11-29T08:32:34Z | |
dc.date.issued | 2022-05-27 | |
dc.description.abstract | Following the 2022 Tonga Volcano eruption, dramatic suppression and deformation of the
equatorial ionization anomaly (EIA) crests occurred in the American sector ∼14,000 km away from the
epicenter. The EIA crests variations and associated ionosphere-thermosphere disturbances were investigated
using Global Navigation Satellite System total electron content data, Global-scale Observations of the Limb
and Disk ultraviolet images, Ionospheric Connection Explorer wind data, and ionosonde observations. The
main results are as follows: (a) Following the eastward passage of expected eruption-induced atmospheric
disturbances, daytime EIA crests, especially the southern one, showed severe suppression of more than 10
TEC Unit and collapsed equatorward over 10° latitudes, forming a single band of enhanced density near the
geomagnetic equator around 14–17 UT, (b) Evening EIA crests experienced a drastic deformation around
22 UT, forming a unique X-pattern in a limited longitudinal area between 20 and 40°W. (c) Thermospheric
horizontal winds, especially the zonal winds, showed long-lasting quasi-periodic fluctuations between
±200 m/s for 7–8 hr after the passage of volcano-induced Lamb waves. The EIA suppression and X-pattern
merging was consistent with a westward equatorial zonal dynamo electric field induced by the strong zonal
wind oscillation with a westward reversal. | en_US |
dc.identifier.citation | Aa, Zhang, Wang, Erickson, Qian, Eastes, Harding, Immel, Karan, Daniell, Coster, Goncharenko, Vierinen, Cai, Spicher. Pronounced Suppression and X-Pattern Merging of Equatorial Ionization Anomalies After the 2022 Tonga Volcano Eruption. Journal of Geophysical Research (JGR): Space Physics. 2022;127(6) | en_US |
dc.identifier.cristinID | FRIDAID 2045656 | |
dc.identifier.doi | 10.1029/2022JA030527 | |
dc.identifier.issn | 2169-9380 | |
dc.identifier.issn | 2169-9402 | |
dc.identifier.uri | https://hdl.handle.net/10037/27578 | |
dc.language.iso | eng | en_US |
dc.publisher | Wiley | en_US |
dc.relation.journal | Journal of Geophysical Research (JGR): Space Physics | |
dc.rights.accessRights | openAccess | en_US |
dc.rights.holder | Copyright 2022 The Author(s) | en_US |
dc.rights.uri | https://creativecommons.org/licenses/by-nc/4.0 | en_US |
dc.rights | Attribution-NonCommercial 4.0 International (CC BY-NC 4.0) | en_US |
dc.title | Pronounced Suppression and X-Pattern Merging of Equatorial Ionization Anomalies After the 2022 Tonga Volcano Eruption | en_US |
dc.type.version | publishedVersion | en_US |
dc.type | Journal article | en_US |
dc.type | Tidsskriftartikkel | en_US |
dc.type | Peer reviewed | en_US |