Gravity waves generated by the Hunga Tonga-Hunga Ha′apai volcanic eruption and their global propagation in the mesosphere/lower thermosphere observed by meteor radars and modeled with the High-Altitude general Mechanistic Circulation Model

Gunter Stober, Sharon L. Vadas, Erich Becker, Alan Liu, Alexander Kozlovsky, Diego Janches, Zishun Qiao, Witali Krochin, Guochun Shi, Wen Yi, Jie Zeng, Peter Brown, Denis Vida, Neil Hindley, Christoph Jacobi, Damian Murphy, Ricardo Buriti, Vania Andrioli, Paulo Batista, John MarinoScott Palo, Denise Thorsen, Masaki Tsutsumi, Njål Gulbrandsen, Satonori Nozawa, Mark Lester, Kathrin Baumgarten, Johan Kero, Evgenia Belova, Nicholas Mitchell, Tracy Moffat-Griffin, Na Li

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Abstract

The Hunga Tonga-Hunga Ha′apai volcano erupted on 15 January 2022, launching Lamb waves and gravity waves into the atmosphere. In this study, we present results using 13 globally distributed meteor radars and identify the volcanogenic gravity waves in the mesospheric/lower thermospheric winds. Leveraging the High-Altitude Mechanistic general Circulation Model (HIAMCM), we compare the global propagation of these gravity waves. We observed an eastward-propagating gravity wave packet with an observed phase speed of 2405.7gmgs-1 and a westward-propagating gravity wave with an observed phase speed of 166.56.4gmgs-1. We identified these waves in HIAMCM and obtained very good agreement of the observed phase speeds of 239.54.3 and 162.26.1gmgs-1 for the eastward the westward waves, respectively. Considering that HIAMCM perturbations in the mesosphere/lower thermosphere were the result of the secondary waves generated by the dissipation of the primary gravity waves from the volcanic eruption, this affirms the importance of higher-order wave generation. Furthermore, based on meteor radar observations of the gravity wave propagation around the globe, we estimate the eruption time to be within 6gmin of the nominal value of 15 January 2022 04:15gUTC, and we localized the volcanic eruption to be within 78gkm relative to the World Geodetic System 84 coordinates of the volcano, confirming our estimates to be realistic.

Original languageEnglish
Pages (from-to)4851-4873
Number of pages23
JournalAtmospheric Chemistry and Physics
Volume24
Issue number8
DOIs
Publication statusPublished - 24 Apr 2024

Data Availability Statement

HIAMCM wind fields can be requested from Sharon L. Vadas ([email protected]). The meteor radar data can be requested from the instrument principal investigators for DAV ([email protected]), TDF ([email protected]), ROT ([email protected]), SVA, and Nordic (consisting of TRO, SOD, ALT, and KIR). ([email protected], [email protected], [email protected], [email protected]), McM ([email protected]), ALO ([email protected]), Poker Flat ([email protected]), CMO ([email protected]), and for CAR ([email protected], [email protected], [email protected]). The Mengcheng and Kunming radar data were provided through Wen Yi ([email protected]). The retrieved 10 min winds can be requested from the University of Bern ([email protected]).

Funding

Operation of the Davis meteor radar was supported by Australian Antarctic Science projects 4445 and 4637. Support for Diego Janches as well as SAAMER-OS' operation are provided by NASA's Planetary Science Division Research Program, through ISFM work packet Exospheres, Ionospheres, Magnetospheres Modeling at Goddard Space Flight Center and NASA Engineering Safety Center (NESC) assessment TI-17-01204. This work was supported in part by the NASA Meteoroid Environment Office under cooperative agreement no. 80NSSC21M0073. Alan Liu is the CONDOR instrument principal investigator, and his work is supported by (while serving at) the National Science Foundation (NSF), USA. Zishun Qiao and the operation of the CONDOR meteor radar system are supported by NSF grant AGS-1828589. This research has been supported by the Schweizerischer Nationalfonds zur F\u00F6rderung der Wissenschaftlichen Forschung (grant no. 200021-200517/1), the National Science Foundation (grant nos. AGS-1832988, AGS-1828589), the National Natural Science Foundation of China (grant no. 42174183), the Science and Technology Facilities Council (grant no. ST/W00089X/1), the Japan Society for the Promotion of Science (grant nos. 21H04516, 21H04518, 21H01144, and 20K20940), the Australian Antarctic Division (grant nos. 4445 and 4637), NASA Engineering and Safety Center (grant no. TI-17-01204), NASA Engineering and Safety Center (grant no. 80NSSC21M0073), the US NSF (grant no. AGS-1651464), the Deutsche Forschungsgemeinschaft (grant no. JA 836/47-1), and the International Space Science Institute (ISSI) in Bern (through ISSI International Team project 23-580 \u2013 Meteors and Phenomena at the Boundary between Earth's Atmosphere and Outer Space). This research was supported by the International Space Science Institute (ISSI) in Bern, through ISSI International Team project 23-580 \u2013 Meteors and Phenomena at the Boundary between Earth's Atmosphere and Outer Space. This study is partly supported by Grants-in-Aid for Scientific Research (grant nos. 21H04516, 21H04518, 21H01144, 20K20940) of the Japan Society for the Promotion of Science (JSPS). Poker Flat Meteor Radar is supported by the US NSF (grant no. AGS-1651464). This research has been supported by the STFC (grant no. ST/W00089X/1 to Mark Lester). Sharon L. Vadas and Erich Becker were supported by US National Science Foundation (NSF) grant no. AGS-1832988. Christoph Jacobi acknowledges support by Deutsche Forschungsgemeinschaft (grant no. JA 836/47-1).

FundersFunder number
NASA Meteoroid Environment Office
NASA's Planetary Science Division Research Program
National Science FoundationAGS-1832988, AGS-1828589, AGS-1651464
International Space Science Institute23-580
NASA Engineering and Safety Center80NSSC21M0073, TI-17-01204
Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung200021-200517/1
National Natural Science Foundation of China42174183
Japan Society for the Promotion of Science20K20940, 21H01144, 21H04516, 21H04518
Australian Antarctic Division4445, 4637
Science and Technology Facilities CouncilST/W00089X/1
Deutsche ForschungsgemeinschaftJA 836/47-1

ASJC Scopus subject areas

  • Atmospheric Science

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