Destructive potential of planetary meteotsunami waves beyond the Hunga Tonga–Hunga Ha’apai volcano eruption

Worldwide tsunamis driven by atmospheric waves – or planetary meteotsunami waves – are extremely rare events. They mostly occur during supervolcano explosions or asteroid impacts capable to generate atmospheric acoustic-gravity waves including the Lamb waves that can circle the globe multiple times. Recently, such ocean waves have been globally recorded after the Hunga Tonga–Hunga Ha’apai volcano eruption on 15 January 2022, but did not pose any serious danger to the coastal communities. However, this study highlights that the mostly ignored destructive potential of planetary meteotsunami waves can be compared to the well-studied tsunami hazards. In practice, several process-oriented numerical experiments are designed to force a global ocean model with the realistic atmospheric response to the Hunga Tonga–Hunga Ha’apai event rescaled in speed and amplitude. These simulations demonstrate that the meteotsunami surges can be higher than 1 m (and up to 10 m) along more than 7 % of the world coastlines. Planetary meteotsunami waves thus have the potential to cause serious coastal damages and even human casualties during volcanic explosions or asteroid impacts either releasing intense acoustic energy or producing internal atmospheric gravity waves triggering the deep-ocean Proudman resonance at a speed of ~212 m/s. Based on records of catastrophic events in the Earth’s history, both scenarios are found to be realistic and, consequently, the global meteotsunami hazards should now be properly assessed to prepare for the next big volcanic eruption or asteroid impact even occurring inland.

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

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

[3]  J. Morgan,et al.  The Chicxulub impact and its environmental consequences , 2022, Nature Reviews Earth & Environment.

[4]  M. Marcos,et al.  Numerical Simulation of Atmospheric Lamb Waves Generated by the 2022 Hunga‐Tonga Volcanic Eruption , 2022, Geophysical Research Letters.

[5]  G. Harrison Pressure anomalies from the January 2022 Hunga Tonga‐Hunga Ha'apai eruption , 2022, Weather.

[6]  D. Themens,et al.  Global Propagation of Ionospheric Disturbances Associated With the 2022 Tonga Volcanic Eruption , 2022, Geophysical Research Letters.

[7]  I. Vilibić,et al.  Meteotsunamis in Orography‐Free, Flat Bathymetry and Warming Climate Conditions , 2022, Journal of Geophysical Research: Oceans.

[8]  M. Marcos,et al.  Numerical simulation of atmospheric Lamb waves , 2022 .

[9]  T. Shepherd,et al.  Waves and coherent flows in the tropical atmosphere: New opportunities, old challenges , 2021, Quarterly Journal of the Royal Meteorological Society.

[10]  I. Vilibić,et al.  Meteotsunamis in Orography-Free, Flat Bathymetry and Warming Climate Conditions , 2021 .

[11]  N. Žagar,et al.  A high‐accuracy global prognostic model for the simulation of Rossby and gravity wave dynamics , 2021, Quarterly Journal of the Royal Meteorological Society.

[12]  M. Dragoni,et al.  A model for the atmospheric shock wave produced by a strong volcanic explosion , 2020 .

[13]  W. Pringle Global Storm Tide Modeling on Unstructured Meshes with ADCIRC v55 - Simulation Results and Model Setup , 2020 .

[14]  X. Huan,et al.  Uncertainty Propagation Using Polynomial Chaos Expansions for Extreme Sea Level Hazard Assessment: The Case of the Eastern Adriatic Meteotsunamis , 2020, Journal of Physical Oceanography.

[15]  R. Cienfuegos,et al.  History and features of trans-oceanic tsunamis and implications for paleo-tsunami studies , 2020 .

[16]  A. Rabinovich Twenty-Seven Years of Progress in the Science of Meteorological Tsunamis Following the 1992 Daytona Beach Event , 2019, Pure and Applied Geophysics.

[17]  I. Vilibić,et al.  The Adriatic Sea and Coast modelling suite: Evaluation of the meteotsunami forecast component , 2019, Ocean Modelling.

[18]  Chin H. Wu,et al.  Unexpected rip currents induced by a meteotsunami , 2019, Scientific Reports.

[19]  anonymous OceanMesh2D 1.0: MATLAB-based software for two-dimensional unstructured mesh generation in coastal ocean modeling , 2018 .

[20]  C. Pattiaratchi,et al.  Are meteotsunamis an underrated hazard? , 2015, Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences.

[21]  E. Okal,et al.  Sequencing of tsunami waves: why the first wave is not always the largest , 2015 .

[22]  Y. Hironaka,et al.  Production of sulphate-rich vapour during the Chicxulub impact and implications for ocean acidification , 2014 .

[23]  I. Vilibić Numerical simulations of the Proudman resonance , 2008 .

[24]  Costas E. Synolakis,et al.  Far-field tsunami hazard from mega-thrust earthquakes in the Indian Ocean , 2008 .

[25]  Vasily Titov,et al.  The Global Reach of the 26 December 2004 Sumatra Tsunami , 2005, Science.

[26]  Efim Pelinovsky,et al.  Asteroid impact tsunamis , 2005 .

[27]  Ira Didenkulova,et al.  Analysis of Tide-Gauge Records of the 1883 Krakatau Tsunami , 2005 .

[28]  Clive Oppenheimer,et al.  The size and frequency of the largest explosive eruptions on Earth , 2004 .

[29]  Efim Pelinovsky,et al.  Simulation of the trans-oceanic tsunami propagation due to the 1883 Krakatau volcanic eruption , 2003 .

[30]  S. Cox,et al.  Exponential Time Differencing for Stiff Systems , 2002 .

[31]  D. Lowe,et al.  Volcano-meteorological tsunamis, thec. AD 200 Taupo eruption (New Zealand) and the possibility of a global tsunami , 2000 .

[32]  J. Forbes,et al.  Lamb waves in the lower thermosphere: Observational evidence and global consequences , 1999 .

[33]  D. Hunten,et al.  IMPACT-INDUCED PERTURBATIONS OF ATMOSPHERIC SULFUR , 1996 .

[34]  Walter H. F. Smith,et al.  A global, self‐consistent, hierarchical, high‐resolution shoreline database , 1996 .

[35]  David Morrison,et al.  Impacts on the Earth by asteroids and comets: assessing the hazard , 1994, Nature.

[36]  C. Chyba,et al.  The 1908 Tunguska explosion: atmospheric disruption of a stony asteroid , 1993, Nature.

[37]  Dick Dee,et al.  An analysis of the vertical structure equation for arbitrary thermal profiles , 1989 .

[38]  S. Self,et al.  The 1883 eruption of Krakatau , 1981, Nature.

[39]  A. Kasahara,et al.  Numerical Integration of the Global Barotropic Primitive Equations with Hough Harmonic Expansions , 1977 .

[40]  K. Yeh,et al.  Acoustic‐gravity waves in the upper atmosphere , 1974 .

[41]  F. Bretherton Lamb waves in a nearly isothermal atmosphere , 1969 .

[42]  F. Press,et al.  Air-Sea Waves from the Explosion of Krakatoa , 1966, Science.

[43]  F. Press,et al.  Propagation of acoustic-gravity waves in the atmosphere , 1962 .

[44]  C. Pekeris,et al.  Atmospheric Oscillations , 1936, Nature.

[45]  Geoffrey Ingram Taylor,et al.  Waves and tides in the atmosphere , 1929 .

[46]  J. Proudman The Effects on the Sea of Changes in Atmospheric Pressure , 1929 .