Marie Bouillon
LATMOS/IPSL, Sorbonne Université, UVSQ, CNRS, Paris, France, LATMOS/IPSL, Sorbonne Université, UVSQ, CNRS, Paris, France
Author ProfileAbstract
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 > 50km 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 waves5,6 propagating at phase speeds of 318.2+/-6 ms-1 at
surface level and between 308+/-5 to 319+/-4 ms-1 in the stratosphere,
and gravity waves propagating at 238+/-3 to 269+/-3 ms-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. 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.