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Tonga volcano eruption trigged atmospheric gravity waves that reached the edge of space
by Staff Writers
Bath UK (SPX) Jul 01, 2022

A view of the volcano's explosion into space as captured by China's FY-4B EO satellite.

The eruption of the Hunga Tonga-Hunga Ha'apai submarine volcano in January 2022 was one of the most explosive volcanic events of the modern era, a new study has confirmed.

Led by researchers from the University of Bath and published in Nature, the study combines extensive satellite data with ground-level observations to show that the eruption was unique in observed science in both its magnitude and speed, and in the range of the fast-moving gravity and atmospheric waves it created.

Following a series of smaller events beginning in December 2021, Hunga Tonga erupted on 15 January this year, producing a vertical plume that extended more than 50km (30 miles) above the surface of the earth. Heat released from water and hot ash in the plume remained the biggest source of gravity waves on earth for the next 12 hours. The eruption also produced ripple-like gravity waves that satellite observations show extended across the Pacific basin.

The eruption also triggered waves in our atmosphere that reverberated around the planet at least six times and reached close to their theoretical maximum speeds - the fastest ever seen within our atmosphere, at 320m per second or 720 miles per hour.

The fact that a single event dominated such a large region is described by the paper's authors as unique in the observational record, and one that will help scientists improve future atmospheric weather and climate models.

Dr Corwin Wright, a Royal Society University Research Fellow based at the Centre for Space, Atmospheric and Oceanic Science at the University of Bath, is the paper's lead author. He said: "This was a genuinely huge explosion, and truly unique in terms of what's been observed by science to date. We've never seen atmospheric waves going round the whole world before, or at this speed - they were travelling very close to the theoretical limit.

"The eruption was an amazing natural experiment. The data we've been able to gather on it will enhance our understanding of our atmosphere and will help us improve our weather and climate models."

Co-author Dr Scott Osprey from the National Centre for Atmospheric Science, based within the Department of Physics, University of Oxford, expects to see further impacts from the Hunga Tonga eruption: "Our study nicely shows how the striking display of global waves is driven by the huge amounts of seawater vaporised during the eruption. However, my gut feeling is that there is more to come from this eruption. As the exceptional amount of water vapour spreads throughout the stratosphere, eyes will turn to the Antarctic ozone hole and just how severe it will be in the spring."

Researchers from the University of Bath, Oxford University, North West Research Associates, University of Massachusetts Lowell, Forschungszentrum Juelich, AIRES, Sorbonne Universite, Virginia Tech, Raytheon Technologies, University of Colorado and NASA worked on the study.

The researchers received funding from the Natural Environment Research Council, Royal Society, NASA, and European Research Council.

The Bath researchers are now focusing on working with colleagues at weather and climate forecasting centres to see how the information gathered from the eruption can be used to make predictions better in future.

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


Related Links
University of Bath
Bringing Order To A World Of Disasters
When the Earth Quakes
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SHAKE AND BLOW
Iceland volcano eruption opens a rare window into the Earth beneath our feet
Uppsala, Sweden (SPX) Jun 30, 2022
The recent Fagradalsfjall eruption in the southwest of Iceland has enthralled the whole world, including nature lovers and scientists alike. The eruption was especially important as it provided geologists with a unique opportunity to study magmas that were accumulated in a deep crustal magma reservoir but ultimately derived from the Earth's mantle (below 20 km). A research team from University of Oregon, Uppsala University, University of Iceland, and Deutsches GeoForschungsZentrum (GFZ) took this ... read more

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