Solid Earth–atmosphere interaction forces during the 15 January 2022 Tonga eruption

Rapid venting of volcanic material during the 15 January 2022 Tonga eruption generated impulsive downward reaction forces on the Earth of ~2.0 × 1013 N that radiated seismic waves observed throughout the planet, with ~25 s source bursts persisting for ~4.5 hours. The force time history is determined by analysis of teleseismic P waves and Rayleigh waves with periods approximately <50 s, providing insight into the overall volcanic eruption process. The atmospheric acoustic-gravity Lamb wave expanding from the eruption produced broadband ground motions when transiting land, along with driven and conventional tsunami waves. Atmospheric standing acoustic waves near the source produced oscillatory peak forces as large as 4 × 1012 N, exciting resonant solid Earth Rayleigh wave motions at frequencies of 3.7 and 4.6 mHz.

[1]  G. Haralabus,et al.  The Hunga Tonga–Hunga Ha’apai Eruption of 15 January 2022: Observations on the International Monitoring System (IMS) Hydroacoustic Stations and Synergy with Seismic and Infrasound Sensors , 2022, Seismological Research Letters.

[2]  C. Synolakis,et al.  Diverse tsunamigenesis triggered by the Hunga Tonga-Hunga Ha’apai eruption , 2022, Nature.

[3]  C. Clerbaux,et al.  Surface-to-space atmospheric waves from Hunga Tonga–Hunga Ha’apai eruption , 2022, Nature.

[4]  P. González,et al.  Global Tonga tsunami explained by a fast-moving atmospheric source , 2022, Nature.

[5]  Jonathan O’Callaghan Burst of underwater explosions powered Tonga volcano eruption. , 2022, Nature.

[6]  A. Komjathy,et al.  Atmospheric waves and global seismoacoustic observations of the January 2022 Hunga eruption, Tonga , 2022, Science.

[7]  Tatsuhiko Saito,et al.  Global fast-traveling tsunamis driven by atmospheric Lamb waves on the 2022 Tonga eruption , 2022, Science.

[8]  D. Dingwell,et al.  Magma Fragmentation , 2022, Reviews in Mineralogy and Geochemistry.

[9]  K. Mandli,et al.  Under the Surface: Pressure-Induced Planetary-Scale Waves, Volcanic Lightning, and Gaseous Clouds Caused by the Submarine Eruption of Hunga Tonga-Hunga Ha’apai Volcano Provide an Excellent Research Opportunity , 2022, Earthquake Research Advances.

[10]  D. Adam Tonga volcano eruption created puzzling ripples in Earth’s atmosphere , 2022, Nature.

[11]  S. Cronin,et al.  Post-caldera volcanism reveals shallow priming of an intra-ocean arc andesitic caldera: Hunga volcano, Tonga, SW Pacific , 2022, Lithos.

[12]  P. Segall,et al.  Repeating caldera collapse events constrain fault friction at the kilometer scale , 2021, Proceedings of the National Academy of Sciences.

[13]  Jing Wang Non-convex ℓ p regularization for sparse reconstruction of electrical impedance tomography , 2020 .

[14]  H. Kanamori,et al.  The 22 December 2018 tsunami from flank collapse of Anak Krakatau volcano during eruption , 2020, Science Advances.

[15]  A. Neri,et al.  Conduit stability effects on intensity and steadiness of explosive eruptions , 2018, Scientific Reports.

[16]  G. Ekström Love and Rayleigh phase-velocity maps, 5–40 s, of the western and central USA from USArray data , 2014 .

[17]  Arnau Folch,et al.  Density‐driven transport in the umbrella region of volcanic clouds: Implications for tephra dispersion models , 2013 .

[18]  Lion Krischer,et al.  ObsPy: A Python Toolbox for Seismology , 2010 .

[19]  P. Papale Strain-induced magma fragmentation in explosive eruptions , 1999, Nature.

[20]  Masayuki Kikuchi,et al.  Inversion of complex body waves , 1982 .

[21]  D. L. Anderson,et al.  Preliminary reference earth model , 1981 .