SunLive – Tonga eruption confirmed as largest ever recorded

NIWA scientists have also unraveled one of the biggest unknowns of the eruption – the pyroclastic flows.

Pyroclastic flows are currents made up of dense lava, volcanic ash, and gases which can reach temperatures of 1000°C and speeds of 700km/hr.

NIWA collected 150 sediment cores which were sent to New Zealand’s University of Otago and the National Oceanographic Center in the UK for analysis.

These samples showed pyroclastic deposits some 80 km away from the volcano.

But Dr Emily Lane, NIWA Principal Scientist – Natural Hazards, believes they could have traveled even further.

“Eighty kilometers was the end of our survey range, but the pyroclastic flows appear to extend beyond that distance, perhaps as far as 100km away. They are also what caused both the domestic and international communications cables to break, with the domestic cable now being buried under 30m of eruptive material.

“The sheer force of the flows is astonishing – we saw deposits in valleys beyond the volcano, which is where the international cable lies, meaning they had enough power to flow uphill over huge ridges and then back down again.”

On land, the heat from pyroclastic flows creates a frictionless boundary layer which allows them to move so rapidly, like how a puck glides on an air hockey table.

However, Kevin says this is the first time that scientists have observed underwater pyroclastic flows of this magnitude.

“It’s the interaction with water that made this event so unprecedented. It’s still speculation but the latest science shows that this phenomenon may be more exaggerated under water. This could be why the pyroclastic flow traveled so far and with such force.”

When heated, water can expand to around 1,000 times its volume. When you get several km 3 of hot magma instantly hitting the cold saltwater, this reaction is supercharged, and all that energy must go somewhere – and the only options are to explode up or sideways out of the volcano.

“While this eruption was large – one of the biggest since Krakatoa in 1883 – there have been others of similar magnitude since then that didn’t behave in the same way. The difference here is that it’s an underwater volcano and it’s also part of the reason we got such big tsunami waves,” said Mackay.

Emily says because these volcanoes are not just found in the Pacific, but the world over, we must know what happened and why it was so violent.

“The pressure anomaly generated by this eruption supercharged the tsunami so that it was able to travel right across the Pacific and world-wide. This mechanism meant that it could travel further and faster than our warning systems expected. The Krakatoa eruption was that last time a volcanic tsunami on this scale occurred.”

The significant reshaping of the seafloor also had dramatic effects on ecosystems in the region.

There was little sign of any animal life on the flanks of the volcano, in deeper water channels, and most of the surrounding seafloor.

However, there were patches of abundant life that had survived the eruption on several seamounts, giving hope for recovery.

This video, shot on board NIWA’s Research Vessel Tangaroa , shows the scale of the HT-HH explosion and the findings of the resulting undersea investigations:

This work was done by the NIWA-Nippon Foundation Tonga Eruption Seabed Mapping Project (TESMaP).

Supported by The Nippon Foundation, NIWA and SEA-KIT surveyed over 22,000km 2 surrounding the volcano, including mapping 14,000km 2 of previously unmapped seafloor as part of The Nippon Foundation GEBCO Seabed 2030 project, which aims to map the world’s oceans by the end of the decade.

Mitsuyuki Unno, Executive Director of The Nippon Foundation, says this work is vital to understand the science behind these types of events.

“The research has made clear that underwater volcanic eruptions have serious implications for coastal communities around the world.

“A huge proportion of the Earth’s population lives on the coast, which are already vulnerable to the impacts of climate change, sea level rise, and big storms.

“We need to further our understanding of the risks from underwater volcanoes so we can better prepare and protect future generations and their ecological environments.”

Jamie McMichael-Phillips, Project Director of The Nippon Foundation GEBCO Seabed 2030 project, says this project highlights the benefits of working in collaboration to collect fundamental knowledge of the ocean seabed.

“TESMaP is a fantastic testament to what can be achieved if we all come together in pursuit of scientific research.

“A complete map of the ocean floor is a necessity to protect our planet in line with the UN SDGs and our Seabed 2030 partners play an invaluable role in helping us realize our goal – as demonstrated by the truly collaborative nature of TESMaP.”

Ben Simpson, CEO of SEA-KIT, says their technology allowed scientists to undertake a dangerous and vital mission.

“We have been able to add new equipment to our proven X-Class Uncrewed Surface Vessel’s survey platform, such as winch and sensor cage towing capability, showing yet again the potential of uncrewed vessel technology to support and develop our understanding of the ocean. USV ‘Maxlimer’ provided a low risk, non-invasive survey solution for this challenging location, bringing down both risk and costs and reducing carbon emissions.”

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