Researchers found a unique seismic signal just before the January 2022 eruption of the Hunga Tonga-Hunga Ha’apai volcano, potentially offering early warnings for oceanic eruptions.
By analyzing a Rayleigh wave detected 750 kilometers away, scientists suggest that a crustal fracture allowed seawater to mix with magma, triggering the eruption.
Early Warning From Seismic Waves
Just fifteen minutes before the massive January 2022 eruption of the Hunga Tonga-Hunga Ha’apai volcano, a seismic wave was recorded by two distant monitoring stations. Researchers now believe that these early signals could help predict similar eruptions in other remote oceanic volcanoes.
According to the researchers, this seismic wave likely resulted from a fracture in a weak area of oceanic crust beneath the volcano’s caldera wall. This fracture allowed seawater and magma to mix in the space above the volcano’s subsurface magma chamber, triggering a powerful explosive reaction that set off the eruption.
The study, published in Geophysical Research Letters, offers new insights into the warning signs of volcanic eruptions. The journal, an open-access publication from the American Geophysical Union, focuses on high-impact reports with immediate relevance to Earth and space sciences.
Potential for Disaster Mitigation
The results build on the researchers’ previous work monitoring remote volcanoes. In this case, the Rayleigh wave, a type of seismic wave that moves through the Earth’s surface, was detected 750 kilometers (approximately 466 miles) from the volcano.
“Early warnings are very important for disaster mitigation,” said Mie Ichihara, a volcanologist at the University of Tokyo and one of the study’s co-authors. “Island volcanoes can generate tsunamis, which are a significant hazard.”
Silent Precursor to a Violent Eruption
Hunga Tonga-Hunga Ha’apai is an oceanic volcano in the western Pacific Ocean in the Kingdom of Tonga. The seamount was created by the subduction of the Pacific Plate underneath the Australian Plate, a process that generates magma and leads to eruptions.
On January 15, 2022, the volcano erupted with record-breaking energy, injecting 58,000 Olympic swimming pools of water vapor into the stratosphere, setting off an unprecedented lightning storm and generating a tsunami. That massive eruption was preceded by a smaller eruption on January 14 and, before that, a month of eruptive activity.
Researchers still debate the exact start time of the eruption, though most agree that the eruption started shortly after 4:00 Coordinated Universal Time (UTC). The new study reports a Rayleigh wave that started around 3:45 UTC.
Rayleigh Wave Detection
The researchers used seismic data to analyze the Rayleigh wave, which was detected by instruments, but not felt by humans, at seismic stations on the islands of Fiji and Futuna. While Rayleigh waves are a common feature of volcanic eruptions and earthquakes, the researchers believe that this wave signified a precursor event and a possible cause of the massive eruption.
“Many eruptions are preceded by seismic activity,” said Takuro Horiuchi, a volcanology graduate student at the University of Tokyo and the lead author of the study. “However, such seismic signals are subtle and only detected within several kilometers of the volcano.”
In contrast, this seismic signal traveled a great distance, indicating a huge seismic event. “We believe unusually large movements started at the time of the precursor,” Horiuchi said.
Secrets of the Seamount
Scientists may never know exactly what caused the gigantic, “caldera-forming” eruption, but Ichihara believes that the process was not instantaneous. Instead, she thinks that this precursor event was the start of an underground process that ultimately led to the eruption.
But it can be difficult to nail down the origins of these rare, colossal eruptions.
“There are very few observed caldera-forming eruptions, and there are even fewer witnessed caldera-forming eruptions in the ocean,” Ichihara said. “This gives one scenario about the processes leading to caldera formation, but I wouldn’t say that this is the only scenario.”
Regardless, detecting early eruption signals may give island nations and coastal areas more valuable time to prepare when faced with imminent tsunamis — even when the signal cannot be felt on the surface.
“At the time of the eruption, we didn’t think of using this kind of analysis in real-time,” Ichihara said. “But maybe the next time that there is a significant eruption underwater, local observatories can recognize it from their data.”
Reference: “A Seismic Precursor 15 min Before the Giant Eruption of Hunga Tonga-Hunga Ha’apai Volcano on 15 January 2022” by Takuro Horiuchi, Mie Ichihara, Kiwamu Nishida and Takayuki Kaneko, 4 November 2024, Geophysical Research Letters.
DOI: 10.1029/2024GL111144