Models underestimated Tonga shockwave

The volcanic eruption in Tonga this month unleashed an atmospheric shockwave that radiated out at close to the speed of sound, pushing large waves across the Pacific to the shores of Japan and Peru, thousands of kilometres away.

Forecasting models and warning systems, designed primarily to assess earthquake-triggered waves, did not account for the boosting effects of the shockwave.

It was a critical flaw in these systems, scientists said, leaving them unable to predict exactly when the waves would hit land.

"The trans-Pacific and global waves arrived earlier than forecast, which (was) terrible for distant shorelines," said civil engineer Hermann Fritz at Georgia Tech University, who studies tsunamis.

The Hunga Tonga-Hunga Ha'apai volcano eruption triggered a tsunami that destroyed villages and resorts and knocked out communications for the South Pacific country of about 105,000 people.

Three people have been reported killed.

However Tongans were well equipped to deal with the tsunami.

The country is considered among the most prepared for natural disasters, with years of tsunami drills under its belt, and many people knew to move to higher ground.

But for faraway Peru, for example, the lack of accurate information may have contributed to the death of two people who drowned in unusually high waves as well as the catastrophic oil spill from a ship near La Pampilla refinery.

"We need to re-evaluate tsunami hazards for other volcanoes around the world," Fritz said.

For example, the underwater volcano known as Kick'em Jenny is thought to pose only a regional tsunami risk to the neighbouring Caribbean island of Grenada.

But in fact "it may very well excite the entire Caribbean and Gulf of Mexico, and possibly even the Atlantic and global oceans, if a Tonga-type event were to happen," he said.

Volcano-triggered tsunamis have been rare in modern history and the shockwave from Tonga's volcano was among the largest ever recorded, similar to the one produced by the 1883 eruption of Krakatoa.

Prior to the 2018 tsunami that followed the eruption of Anak Krakatau, a tsunami set off by a volcano had not happened in the ocean in more than a century.

Rather, 90 per cent of tsunamis are triggered by earthquakes.

As such, tsunami warning systems are programmed to prioritise seismic events, with scientists gauging risk by whether an earthquake magnitude is high enough - above 7.5 on the Richter scale - to cause a destructive tsunami.

Seafloor instruments also monitor for irregular changes in wave height, sending information by surface buoy and then satellite to a warning centre for assessment.

The Pacific Tsunami Warning Center in Hawaii initially warned of dangerous waves within 1000km of the Tonga eruption.

However, their bulletin noted that "due to the volcano source we cannot predict tsunami amplitudes nor how far the tsunami hazard may extend".

Roughly 10 hours later, the warning was updated to include a possible threat to Peru - a surprising development given that the tsunami near Tonga was relatively small.

Tsunami waves, driven by gravity, travel at about 200 metres per second - roughly the speed of a jetliner.

But the shockwave from Tonga's volcano had moved at more than 300 metres per second and was so powerful, scientists said, that it caused the atmosphere to ring like a bell.

Through the transfer of this energy from the atmosphere to the ocean, the shockwave amplified ocean waves around the world, pushing them farther afield and accelerating their travel time - something tsunami warning centres weren't equipped to handle.

Now, Fritz said, the possibility of atmospheric pressure waves needs to "be added to tsunami warning centres' suite of modelling and forecasting tools".