Home > Publications database > Surface-to-space atmospheric waves from Hunga Tonga-Hunga Ha’apai eruption |
Journal Article | FZJ-2022-02609 |
; ; ; ; ; ; ; ; ; ; ; ; ;
2022
Nature Publ. Group
London [u.a.]
This record in other databases:
Please use a persistent id in citations: http://hdl.handle.net/2128/31901 doi:10.1038/s41586-022-05012-5
Abstract: The January 2022 Hunga Tonga–Hunga Haʻapai eruption was one of the most explosive volcanic events of the modern era, producing a vertical plume which peaked > 50 km above the Earth. The initial explosion and subsequent plume triggered atmospheric waves which propagated around the world multiple times. 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 propagating at phase speeds of 318.2±6 m/s at surface level and between 308±5 to 319±4 m/s in the stratosphere, and gravity waves propagating at 238±3 to 269±3 m/s 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. Latent heat release from the plume remained the most significant individual gravity wave source worldwide for > 12 hours, 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.
The record appears in these collections: |