Lightning Rings and Gravity Waves: Insights Into the Giant Eruption Plume From Tonga's Hunga Volcano on 15 January 2022

Author:

Van Eaton Alexa R.1ORCID,Lapierre Jeff2,Behnke Sonja A.3ORCID,Vagasky Chris45ORCID,Schultz Christopher J.6ORCID,Pavolonis Michael7ORCID,Bedka Kristopher8ORCID,Khlopenkov Konstantin9ORCID

Affiliation:

1. U.S. Geological Survey Cascades Volcano Observatory Vancouver WA USA

2. Advanced Environmental Monitoring (AEM) Germantown MD USA

3. Electromagnetic Sciences and Cognitive Space Applications Los Alamos National Laboratory Los Alamos NM USA

4. Vaisala Inc. Louisville CO USA

5. Now at Department of Agronomy University of Wisconsin Madison WI USA

6. NASA Marshall Space Flight Center Huntsville AL USA

7. National Oceanic and Atmospheric Administration (NOAA)/National Environmental Satellite, Data, and Information Service (NESDIS) Center for Satellite Applications and Research Advanced Satellite Products Branch Madison WI USA

8. NASA Langley Research Center Hampton VA USA

9. Science Systems and Applications, Inc Hampton VA USA

Abstract

AbstractOn 15 January 2022, Hunga Volcano in Tonga produced the most violent eruption in the modern satellite era, sending a water‐rich plume at least 58 km high. Using a combination of satellite‐ and ground‐based sensors, we investigate the astonishing rate of volcanic lightning (>2,600 flashes min−1) and what it reveals about the dynamics of the submarine eruption. In map view, lightning locations form radially expanding rings. We show that the initial lightning ring is co‐located with an internal gravity wave traveling >80 m s−1 in the stratospheric umbrella cloud. Buoyant oscillations of the plume's overshooting top generated the gravity waves, which enhanced turbulent particle interactions and triggered high‐current electrical discharges at unusually high altitudes. Our analysis attributes the intense lightning activity to an exceptional mass eruption rate (>5 × 109 kg s−1), rapidly expanding umbrella cloud, and entrainment of abundant seawater vaporized from magma‐water interaction at the submarine vent.

Funder

U.S. Geological Survey

Los Alamos National Laboratory

Marshall Space Flight Center

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

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