Major Eruption of Undersea Volcano in Tonga

Small update: According to Dr Judith Hubbard, who's associated with Earth Observatory Singapore, there have been dozens of M4.5-5 quakes in the area of the volcano, most likely due to crustal stress caused by the eruption but may also be linked with magma movement, although it's difficult to tell because there are so few seismic networks in the region; that's pretty much all she had to report.

First tweet from a thread of 3 below. Text is pasted from all 3:


The eruption is over but the ground is still shaking - there have been dozens of #earthquakes around the #HungaTonga #volcano (magnitude 4.5-5), continuing today. 1/3

Many are likely due to slip on existing faults or fracturing of new ones due to changes in crustal stress caused by the eruption. Others may be linked to magma movement, although that usually produces a more persistent signal called #volcanictremor. 2/3

haven't seen any focal mechanisms for these events, which would tell us more about the type of #earthquake - it may be difficult to extract that information as these events are M5 or less, and seismic networks are sparse in this region. 3/3
 
Some perspective on how big Tonga really was (hint:massive):
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How big was the Tonga eruption?​

The explosive eruption of the Hunga Tonga-Hunga Ha'apai volcano may be one of the largest recorded in such detail. The blast was visible from space, with images of the massive ash plume going viral over the following days. But just how big was it?
By Manas Sharma and Simon Scarr
PUBLISHED JAN. 21, 2022
The underwater volcano erupted with a deafening explosion on Jan. 15, triggering deadly tsunamis, covering islands in ash, and knocking out communications for Tonga's 105,000 people

The event was captured in astonishing detail by satellites including the NOAA GOES-West satellite, shown below.

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Satellite images: NOAA. Jan. 21, 2022

Breaking down the stages of the eruption into intervals allows us to plot the expansion of the enormous plume of material that volcanologists call an “umbrella cloud”.

Around the time of the initial eruption, a cloud measuring 38 km (24 miles) wide is thrust into the atmosphere. Its diameter already measures almost twice the length of Manhattan, New York. One hour later, it appears to measure around 650 km wide, including shock waves around its edge.




One hour later
18:00
18:10
Initial eruption
Half an hour later
17:40
17:50
17:10
local time
17:20
17:30
120 km
38 km
340 km
Manhattan, NY,
to scale
650 km
The scale of the umbrella cloud is comparable to the 1991 Pinatubo eruption in the Philippines and is one of largest of the satellite era, according to Michigan Tech volcanologist Simon Carn in a NASA blog post.

Different perspectives​



Scientists are still determining the Volcanic Explosivity Index (VEI) of the eruption, a measurement from 1 to 8 that examines the explosivity of eruptions. Pinatubo, which is considered similar to the Hunga Tonga-Hunga Haʻapai eruption, scored a 6 on the index.

Pinatubo produced an eruption column of gas and ash that rose 40 km into the atmosphere, whereas “preliminary data on the Tongan eruption is that the gas and ash column was at least 20 km high,” said Raymod Cas, a volcanologist at Monash University in Australia.

Satellite imagery​

Base maps: NASA, Terra/MODIS

Eruption clouds: NOAA, GOES-West

Note​

All maps and satellite imagery reprojected to orthographic projections for accuracy of measurements

Sources​

NASA; NOAA; Google Earth
 
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Here's another video with the various satellite images and other findings of the blast.

At 1:20 min. radio waves recorded the lightning flashes occurring in the plum with an estimation of approximately 200,000 lightning bolts so this was quite electrical as well.

At 3:50 the infrared detected shock waves are shown that spread around the planet and at the time of this recoding there had been 4 such waves. Weather stations in various countries showed the waves passage in changes in the air pressure.

This is looking cosmic to me....... did this affect the consciousness' of humans and will it alter current events in some way. Was this a blast from 4D? :-D WOW!

 
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Tonga volcano eruption yields insights into asteroid impacts on Earth​


The Hunga Tonga-Hunga Ha'apai volcano eruption is seen from space in this NASA animation.

The Hunga Tonga-Hunga Ha'apai volcano eruption is seen from space in this NASA animation. (Image credit: NASA/NOAA/NESDIS)


On Jan. 15, 2022, the Hunga Tonga-Hunga Ha'apai volcano erupted off the coast of Tonga in the South Pacific Ocean, generating a tsunami and triggering resulting wave action alerts around the world.

The underwater volcanic eruption spewed ash, steam, and gas a radius of over 160 miles (260 kilometers) and more than 12 miles (19 km) into Earth's atmosphere.

An infrasound network operated by the Comprehensive Nuclear-Test-Ban Treaty Organization (CTBTO) found the blast to be the largest incident ever recorded by that monitoring system. All 53 infrasound stations recorded the main eruption, at global ranges. The discharge was much larger than the Chelyabinsk meteor airburst in 2013.

The Tongan government described the eruption an "unprecedented disaster," with the island nation suffering loss of life, major damage to homes and loss of infrastructure.

We now know quite a bit about the undersea upsurge. And there appear to be takeaway messages for those concerned about an impacting space rock and the creation of similar effects. Space.com reached out to noted experts in the asteroid impact field to gauge similarities between an undersea belch and Earth taking an asteroid punch in the oceans.

Indeed, data amassed from the Tonga occasion is keeping the scientific community busy.

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An infrasound station operated by the Comprehensive Nuclear-Test-Ban Treaty Organization (CTBTO). All 53 infrasound stations recorded the main eruption, at global ranges. (Image credit: CTBTO)


Effects and after-effects​


Lindley Johnson is NASA's Planetary Defense Officer in Washington. "We should examine all natural disasters — but both volcanoes and earthquakes in particular — for lessons to be learned about the effects and after-effects of a significant asteroid impact."

Johnson pointed out that there have been suggestions that the Tonga eruption released about the same amount of energy as is estimated for the June 30, 1908 Tunguska impact event in Siberia, Russia. "I don't know how valid that assessment is, but it is certainly worth looking at as an analogy."

"A dangerous asteroid is likely to hit [an] ocean, not land, because over 70% of Earth's surface is ocean. But a disproportionately large fraction of people live near coasts, so tsunamis are a threat,"
Clark Chapman, a senior scientist (retired) from the Southwest Research Institute in Boulder, Colorado, told Space.com.

"We need to learn more about asteroid impact tsunamis, because they probably behave very differently from those caused by earthquakes or landslides," Chapman said.


Risk assessments and simulations​


Lorien Wheeler and colleague Michael Aftosmis work on NASA's Asteroid Threat Assessment Project at the Ames Research Center in California's Silicon Valley. Their research is done under NASA's Planetary Defense Coordination Office.

Wheeler is the risk assessment lead for the project, focused on building fast-running probabilistic models that look at the amount of risk that different asteroid hazards can pose.

Aftosmis is an aerospace engineer in the Advanced Supercomputing Division developing high-fidelity simulations of asteroid strikes, including blast wave propagation, tsunami, thermal and global effects.

The analogy between a volcano and an asteroid hit is not obvious Aftosmis said, as one comes from the ground up the other comes from the outside in. "An undersea volcano and an asteroid impact, they have a lot of similarities when it comes to the kind of tsunami that might be triggered," he said.


Coupling of energy​


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Japan's Himawari 8 satellite imagery captured the Jan. 15, 2022 volcanic eruption in the southwest Pacific. (Image credit: Japan Meteorological Agency)


"When you look at the aggregate level of risk from potential asteroid impacts, considering all the different frequencies of sizes that are most likely to hit us," Wheeler said, "our current models indicate the risk of large tsunamis from asteroid impact is relatively low, compared to other potential impact hazards like local blast, global effects."

However, given a big enough asteroid that strikes close enough to a coastline, it could cause a sizable tsunami, Wheeler said. "It's important to develop good tsunami models to be able to predict those consequences as well as we can."

The Tonga incident may give some insights on the coupling of energy to the atmosphere and water, such as how fast ocean waves dissipate, to better refine simulation models, Wheeler said.

Airblast coupling, the tsunami from the eruption itself and also seismic effects data from the Tonga episode are being studied. While asteroid-generated tsunamis are a relatively small threat contrasted to other effects, this particular case does have some interesting similarities and raises physics questions worthy of pursuit, Aftosmis said.

Furthermore, over several years, there have been a series of "tabletop" exercises hosted jointly by NASA and the Federal Emergency Management Agency (FEMA), held specifically to respond to and better prepare for an asteroid-meets-Earth scenario, if and when emergency action is required.

The upshot from assessing the Tonga event does yield valuable information that could be fed into future tabletop exercises, to better hone ways to estimate the level of risk and better inform response decisions, Wheeler said.



Existence proof​


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Asteroid impact fireball produced from supercomputer simulation run by a Sandia National Laboratories team led by Mark Boslough.
(Image credit: Sandia National Laboratories/Randy Montoya)




Noted asteroid expert Mark Boslough is an adjunct professor in the Department of Earth and Planetary Sciences at the University of New Mexico. He participated in documentary field expeditions to airburst sites including the Libyan Desert of Egypt in 2006, Tunguska in 2008, and Chelyabinsk, Russia in 2013 to assess the impressive Feb. 15, 2013 event when a destructive meteor burst occurred in the atmosphere.

Several years ago, Boslough suggested the potential for asteroid airburst-generated "meteotsunami" — large waves driven by air-pressure disturbances.

As for the Hunga Tonga-Hunga Ha'apai volcano eruption, "yes, this is a great test of the idea, and I understand that meteotsunami were detected in Puerto Rico and Menorca," Boslough said.

It appears to Boslough that these have to be from air-coupled tsunamis as opposed to direct generation at the source of the explosion because they are in different ocean basins.

"If this turns out to be the case, then we now have an 'existence proof' that pressure waves in the atmosphere from big explosions can trigger tsunami far away from the explosion itself. If volcanoes can do this, I think asteroid airbursts can as well," Boslough said.


Leonard David is author of "Moon Rush: The New Space Race" (National Geographic, 2019). A longtime writer for Space.com, David has been reporting on the space industry for more than five decades. Follow us on Twitter @Spacedotcom or on Facebook.
 
BBC news on the Tonga volcano
25 May 2022



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Researchers have just finished mapping the mouth of the underwater Tongan volcano that, on 15 January, produced Earth's biggest atmospheric explosion in over a century.

The caldera of Hunga-Tonga Hunga-Ha'apai is now 4km (2.5 miles) wide and drops to a base 850 m below sea level. Before the catastrophic eruption, the base was at a depth of about 150m.

It drives home the scale of the volume of material ejected by the volcano - at least 6.5 cubic km of ash and rock.
"If all of Tongatapu, the main island of Tonga, was scraped to sea level, it would fill only two-thirds of the caldera," Prof Shane Cronin from the University of Auckland, New Zealand, said.

Prof Cronin has spent the past two and a half months in the Pacific kingdom, seconded to its geological services department.

Their report, issued on Tuesday, assesses the eruption and makes recommendations for future resilience.
Although Hunga-Tonga Hunga-Ha'apai (HTHH) is unlikely to give a repeat performance for many hundreds of years, there are at least 10 volcanic seamounts in the wider region of the south-west Pacific that could produce something similar on a shorter timescale.
New Zealand's National Institute for Water and Atmospheric (NIWA) Research released its bathymetry (depth) map for the area immediately around the volcano, on Monday.

But the agency has yet to take soundings directly over the top of HTHH. So Prof Cronin and colleagues' data literally fills a hole in the NIWA survey.


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"The NIWA released a map of the area around the volcano, this week, but not of its caldera"


A comparison with pre-eruption maps of the caldera, made in 2016 and 2015, shows the major changes.

In addition to a general deepening, big chunks have been lost from the interior cliff walls, particularly at the southern end of the crater.
There is evidence of continued infall of loose material - but on the whole, the volcano cone as it stands today looks structurally sound.

"Eventually, the caldera will be a little bit bigger in diameter and a little bit shallower as the sides collapse inwards," Prof Cronin told BBC News. "So we'll have ongoing interest.

"The north-eastern side looks a bit thin and if that failed, a tsunami would endanger the Ha'apai islands. But the volcano's structure does look pretty robust."

Scientists are beginning to get a good handle on how the eruption progressed - and was powered.

The wealth of observational data from 15 January suggests the event became supercharged in the half-hour after 17:00 local time.

As the caldera cracked, seawater was able to interact with decompressing hot magma being drawn up rapidly from depth.
"There were sonic booms as you got large-scale magma-water interactions," Prof Cronin said. "So an explosion followed by water flushing back in again and then another explosion followed by water flushing back in again, explosion - and away we go... like an engine."


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Prof Cronin highlighted the significance of pyroclastic flows in the eruption.

These thick dense clouds of ash and rock thrown into the sky fall back to roll down the sides of the volcano and along the ocean floor.
They will have caused much of the tsunami wave activity that inundated coastlines across the Tongan archipelago.
Prof Cronin accompanied staff from the Tonga Geological Services department to more than 80 locations on various islands, to document one of the most widespread and destructive tsunami events known from a volcano, with waves running up above:

  • 18m at Kanokupolu, on western Tongatapu (65km south of HTHH)
  • 20m on Nomukeiki Island (a similar distance but to the north-east)
  • 10m on islands at distances greater than 85km from the volcano

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The investigations have informed a report for Tonga's Ministry for Lands and Natural Resources.

Rather than rebuilding like-for-like tourism resorts in low-lying areas, it suggests developing "Mediterranean-style", or "pop-up", day-use beach reserves and parks, with the resort accommodation on higher, more landward sites.

"They should also plant a whole lot more trees, like mango," Prof Cronin said.
"They fall over when the tsunami moves through - but they create these log dams and these really reduce the flow energy of the waves."

NIWA, with a UK partner, Sea-Kit International, will shortly make another caldera map. This will be useful to gauge ongoing sediment movement at the crater edges, and continued low-level venting from inside the volcano.
 


One year ago, the Hunga Tonga-Hunga Ha’apai volcano erupted, causing widespread destruction to the Pacific Island Nation of Tonga. It spewed volcanic material up to 58 km into the atmosphere, brought a nearly 15 m tsunami that crashed ashore, destroying villages, and created a sonic boom that rippled around the world – twice.
Even one year on, interest in the extraordinary explosive eruption remains. A sound artist has recently recreated the sonification of the underwater volcanic eruption using rayleigh signal intensity data provided by the Aeolus Virtual Research Environment platform.
Using wind data obtained on one of its overpasses over the ash cloud of the Hunga Tonga explosion, Jamie Perera used an audio sample of one of the shock waves, time-stretched it into a ghostly tone, and assigned it to harmonic values transcribed from 90 Aeolus readings taken over a duration of approximately 15 minutes.
The listener hears one reading every two seconds, in a harmonic range that spans six piano octaves, the highest of which can be heard at around 01:18 minutes when the readings show the eruption’s dust plume at its highest peak (over 20.5 km). The artistic intention behind the sonification was to evoke the otherworldly landscape of Hunga Tonga and other volcanoes.
Sonification credit/copyright: @jamieperera (2023). Used by permission. Data and guidance provided by Daniel Santillan. Thanks to Peter Bickerton and Jemma Foster. Originally created as part of Wild Alchemy Journal - Air Edition - Aeolus


and from here (original in french) :

"In a recent article published in the journal Nature, a team of scientists showed the unprecedented increase in global stratospheric water mass of 13% (compared to climatological levels) and a five-fold increase in the stratospheric aerosol load – the highest in the last three decades.

Using a combination of satellite data, in addition to data from the Aeolus satellite and ground-based observations, the team found that due to the extreme altitude, the volcanic plume circled the Earth in just one week. and dispersed almost pole to pole in three months.

The unique nature and scale of the global stratospheric disturbance by the Tonga eruption ranks it among the most notable natural events of the modern era of observation."
 


One year ago, the Hunga Tonga-Hunga Ha’apai volcano erupted, causing widespread destruction to the Pacific Island Nation of Tonga. It spewed volcanic material up to 58 km into the atmosphere, brought a nearly 15 m tsunami that crashed ashore, destroying villages, and created a sonic boom that rippled around the world – twice.
Even one year on, interest in the extraordinary explosive eruption remains. A sound artist has recently recreated the sonification of the underwater volcanic eruption using rayleigh signal intensity data provided by the Aeolus Virtual Research Environment platform.
Using wind data obtained on one of its overpasses over the ash cloud of the Hunga Tonga explosion, Jamie Perera used an audio sample of one of the shock waves, time-stretched it into a ghostly tone, and assigned it to harmonic values transcribed from 90 Aeolus readings taken over a duration of approximately 15 minutes.
The listener hears one reading every two seconds, in a harmonic range that spans six piano octaves, the highest of which can be heard at around 01:18 minutes when the readings show the eruption’s dust plume at its highest peak (over 20.5 km). The artistic intention behind the sonification was to evoke the otherworldly landscape of Hunga Tonga and other volcanoes.
Sonification credit/copyright: @jamieperera (2023). Used by permission. Data and guidance provided by Daniel Santillan. Thanks to Peter Bickerton and Jemma Foster. Originally created as part of Wild Alchemy Journal - Air Edition - Aeolus


and from here (original in french) :

"In a recent article published in the journal Nature, a team of scientists showed the unprecedented increase in global stratospheric water mass of 13% (compared to climatological levels) and a five-fold increase in the stratospheric aerosol load – the highest in the last three decades.

Using a combination of satellite data, in addition to data from the Aeolus satellite and ground-based observations, the team found that due to the extreme altitude, the volcanic plume circled the Earth in just one week. and dispersed almost pole to pole in three months.

The unique nature and scale of the global stratospheric disturbance by the Tonga eruption ranks it among the most notable natural events of the modern era of observation."

Well, that was creepy and awesome at the same time. It sounded like the Earth opened its mouth and screamed.
 
Hunga-Tonga Ha’apai Volcano, Tonga - Pacific Ocean
15 Jan 2021 • (133m / 436feet )

I believe something major has happened at the Hunga-Tonga Ha’apai Volcano - and I don't mean the big outbreak from yesterday on 14 January 2022 (actually 13 Jan) which was already large, but a new event this morning (European local time), something major must have happened. As I checked Windy.com after work early this morning - the eruption plume had just started to expand (at sunset, their local time) - and only hours later, it expanded to the size of Northern New Zealand.

I took screen captures of the (ongoing) event, as well a gif animation - which illustrates chillingly how the ash cloud expands, at the same time sends sort of "pressure wave" ripples through the neighboring clouds in a circle over 1600 km in diameter.

That is what let's me assume something far larger must have happened, just hours ago and still ongoing. So far, no reports from that event. But Vulkane.net wrote about the 13 Jan event (se below)

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At german Vulkane.net, Marc Szeglat wrote
There's talk that its the reason for the heavy rain that caused the flooding in NSW Australia.
 
Well, that was creepy and awesome at the same time. It sounded like the Earth opened its mouth and screamed.
Oh la la! This is so of a beautiful sound, and at the same time horrendous.
Fire, rain, wind, all the elements of nature seem to be there, that's what I felt. And then also, as if for a few seconds, hell had opened its doors and allowed demons to come out, and also allowed us to hear screams, screams of horror and suffering. But also I had the impression of listening to the sounds of another planet, or maybe of the earth planet before, when everything was matter, fire, wind… Wow! It's really strange!
 
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