4.8 Article

Surface-to-space atmospheric waves from Hunga Tonga-Hunga Ha'apai eruption

Journal

NATURE
Volume 609, Issue 7928, Pages 741-+

Publisher

NATURE PORTFOLIO
DOI: 10.1038/s41586-022-05012-5

Keywords

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Funding

  1. Royal Society University Research Fellowship [UF160545]
  2. NERC [NE/S00985X/1]
  3. NASA Heliophysics DRIVE Science Center [80NSSC20K0628]
  4. NERC Fellowship [NE/P006450/1]
  5. European Research Council (ERC) under the European Union [742909]
  6. NASA AIM Small Explorer Program [NAS5-03132]
  7. European Research Council (ERC) [742909] Funding Source: European Research Council (ERC)

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The January 2022 Hunga Tonga-Hunga Ha'apai eruption was one of the most explosive volcanic events of the modern era, generating a series of atmospheric waves including Lamb waves at the surface and gravity waves in the stratosphere. This eruption had a global-scale impact and resulted in visible circular wavefronts in satellite observations. It holds significant importance for improving weather and climate models.
The January 2022 Hunga Tonga-Hunga Ha'apai eruption was one of the most explosive volcanic events of the modern era(1,2), producing a vertical plume that peaked more than 50 km above the Earth(3). The initial explosion and subsequent plume triggered atmospheric waves that propagated around the world multiple times(4). A global-scale wave response of this magnitude from a single source has not previously been observed. Here we show the details of this response, using a comprehensive set of satellite and ground-based observations to quantify it from surface to ionosphere. A broad spectrum of waves was triggered by the initial explosion, including Lamb waves(5,6) propagating at phase speeds of 318.2 +/- 6 m s(-1) at surface level and between 308 +/- 5 to 319 +/- 4 m s(-1) in the stratosphere, and gravity waves(7) propagating at 238 +/- 3 to 269 +/- 3 m s(-1) in the stratosphere. Gravity waves at sub-ionospheric heights have not previously been observed propagating at this speed or over the whole Earth from a single source(8,9). Latent heat release from the plume remained the most significant individual gravity wave source worldwide for more than 12 h, producing circular wavefronts visible across the Pacific basin in satellite observations. A single source dominating such a large region is also unique in the observational record. The Hunga Tonga eruption represents a key natural experiment in how the atmosphere responds to a sudden point-source-driven state change, which will be of use for improving weather and climate models.

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