December 2021 After staying relatively inactive since 2014, the Hunga Tonga–Hunga Haʻapai volcano erupted on 20 December 2021, sending particulates into the
stratosphere. A large
plume of ash was visible from
Nukuʻalofa, the capital city of Tonga, about from the volcano. This initial eruption ended at 02:00 on 21 December 2021. On 22 and 23 December 2021, plumes containing
sulfur dioxide drifted to the north-north-east and spread over the
Niuatoputapu,
Haʻapai and
Vavaʻu island groups.
Surtseyan explosions, steam plumes and steam bursts were recorded by a Tonga Navy crew on 23 December 2021, during which time the first ground-based images of the
eruption were created. During 29–30 December 2021, several surges of Surtseyan activity occurred, some of which were witnessed by passengers on a small South Seas Charters boat. Eruption plumes during the second half of December 2021 interrupted air travel to Tonga multiple times. The government of Tonga issued a
tsunami warning to residents, and waves of were observed in Nuku'alofa. Later in the afternoon, Tongan geologists near the volcano observed explosions and a ash column between 17:00 and 18:30 local time. A much larger
Plinian eruption started the following day (15 January 2022) at 17:14 local time (04:14:45
UTC, 15 January). The eruption column from this eruption rose into the
mesosphere. The VAAC again issued an advisory notice to airlines. Ash from the eruption made landfall on the main island of Tongatapu, blotting out the
sun. Loud explosions were heard away in Nukuʻalofa, and small stones and ash rained down from the sky. Many residents in Tonga were stuck in traffic whilst attempting to flee to higher ground. The explosion was heard in
Samoa, roughly away before the sound travelled to more distant countries. Residents in
Fiji, more than away, described the sounds of thunder, while the "thump" of the eruption was also reported in
Niue and
Vanuatu. Tremors and shaking buildings were reported by residents in south-western Niue, around
Alofi and
Avatele. The
United States Geological Survey estimated the eruption at a
surface-wave magnitude of 5.8. A series of bangs were heard around 3:30 a.m. local time in and around
Anchorage, Alaska, approximately away from the volcano, lasting about 30 minutes. Low-frequency noise persisted for approximately two hours. Booms were heard as far away as
Yukon in Canada, away. explosion caused atmospheric
shockwaves to propagate around the globe. Satellites visually captured shockwaves propagating across the Pacific Ocean and a very wide
eruption column. and Australia to 6.9 hPa at
Lord Howe Island and 3.3 hPa at
Perth. Even in Europe, a pressure fluctuation of 2.5 hPa was measured in Switzerland, and of just over 2 hPa when it reached the United Kingdom. Shockwaves were reported as having gone around the Earth as many as four times in Japan and
Utah, and at least twice at the
Blue Hill Meteorological Observatory in
Massachusetts. The pressure shockwave was also observed in
Chennai, India, which is 12,000 km from the eruption site. Intense
lightning activity was recorded during the eruption phase. The Vaisala Global Lightning Dataset GLD360 detected lightning in the form of
radio waves. Several hundred to a thousand flashes of lightning were recorded by the system during the two weeks before the eruption. From 14 to 15 January 2022, tens of thousands of lightning flashes occurred. Preliminary observations showed that the eruption column ejected a large amount of volcanic material into the stratosphere, leading to speculation that it would cause a temporary climate cooling effect. Later calculations showed it injected an estimated 400,000 tonnes of sulfur dioxide into the stratosphere and was unlikely to have any global cooling effect. Despite this, the eruption had a cooling effect in the Southern Hemisphere, causing slight cooling of winters and spectacular sunsets. People living in the Southern Hemisphere experienced purple sunsets for a few months after the eruption. A cooling effect of was expected to last until spring (September–November) 2022. The eruption was described as a once-in-a-thousand-year event for the Hunga caldera. NASA satellite
Aura detected the eruption using its
microwave limb sounder. It measures ozone, water vapor and other atmospheric gases, and can penetrate obstacles such as ash clouds. The underwater explosion also sent 146 million tons of water from the South Pacific Ocean into the stratosphere. The amount of water vapor ejected was 10 percent of the stratosphere's typical stock. It was enough to temporarily warm the surface of Earth. It is estimated that an excess of water vapour should remain for 5–10 years. The initial explosive event was possibly more powerful than the
Hatepe eruption, even though Hatepe ejected over ten times the volume of material in a longer eruption. Hunga Tonga–Hunga Haʻapai erupted over a span of 12 hours, releasing of ejecta with an estimated mass of 2,900
teragrams. Although the eruption energy was soon estimated from the acoustic waves and the ash cloud, its ranking on the Volcanic Explosivity Index (VEI) is still debated. The
ERA paper says the eruption correlated to a VEI of 5–6. An April 2022 research paper led by Poli and Shapiro and published by the
American Geophysical Union indicates that the eruption is the largest ever observed with modern instrumentation and estimates its VEI to be approximately 6. Meanwhile, Vergoz and others estimate the blast yield to be 100–200 megatons of TNT and place the corresponding VEI at 5.8. Likewise, a study by Diaz and Rigby estimates the energetic output of the eruption to be equivalent to 61 megatons of
TNT, making the event more powerful than the largest nuclear bomb ever detonated (
Tsar Bomba). The
Smithsonian Institution Global Volcanism Program rated the eruption at VEI-5, The
ERA paper also concludes that this eruption resulted in the formation of a new caldera. In May 2022, scientists at the
National Institute of Water and Atmospheric Research (NIWA) released a
bathymetry map indicating a large caldera measuring in width formed from the eruption. Surveys also indicated that the caldera floor is located below sea level. According to a volcanologist, the caldera walls continue to experience ongoing collapses. Surveys of the seafloor around the volcano found large sediment piles, layers of fine mud and ash, and valleys up to from the volcano. The survey indicated that an estimated of debris was added to a seafloor. Scientists also suggest that the volcano may still be erupting underwater. A 2022 study in the journal
Ocean Engineering by Heidarzadeh and others determined the size of the initial tsunami caused by the eruption. The study analyzed data from 22 tide gauges, eight
Deep-ocean Assessment and Reporting of Tsunamis (DART) stations, eight atmospheric pressure time series,
spectral analysis and
computer simulation. It was concluded that the eruption displaced 6.6 km3 of seawater, in
amplitude, with a length of . The displacement generated a number of waves in the atmosphere, including
Lamb waves in the troposphere and
gravity waves in higher layers of the atmosphere, which propagated around the world at speeds close to the
speed of sound. In mid-May 2024,
University of Rhode Island oceanographer Roxanne Beinart published a study in the journal
Nature Communications Earth and Environment which concluded that the eruption blanketed the surrounding ocean floor with ash for several months, decimating the local marine wildlife. Beinart had led a research cruise in the South Pacific in April 2022 to research underwater biology living around deep-sea hot springs in the region. She found that the site near the volcano was covered in ash, with some of it even at a depth of underwater. File:Hunga Tonga–Hunga Haʻapai on Sentinel-2 L2A 20 December 2021 (cropped).jpg|Hunga Tonga-Hunga Haʻapai in December 2021 File:Hunga Tonga–Hunga Haʻapai on Sentinel-2 L2A 21 February 2022 (cropped).jpg|Hunga Tonga-Hunga Haʻapai in February 2022, after the eruption
Climate and atmospheric impact The eruption produced a massive
eruption column, reaching heights of and thus breaking into the
mesosphere. This is the highest recorded eruption column since Krakatoa's in 1883, which extended up to high. The column developed two "umbrella"-like clouds, one at in height and the other at , and generated a
terrestrial gamma-ray flash. The column ejected a large quantity of water into the stratosphere, where it disturbed the local temperature balance and caused the formation of anomalous winds. Large volcanic eruptions can inject large amounts of
sulfur dioxide into the stratosphere, causing the formation of
aerosol layers that reflect sunlight and can cause a cooling of the climate. In contrast, during the Hunga Tonga–Hunga Haʻapai eruption this sulfur was accompanied by large amounts of water vapour, which by acting as a
greenhouse gas overrode the aerosol effect and caused a net warming of the climate system. One study estimated a 7% increase in the probability that
global warming will exceed in at least one of the next five years, although greenhouse gas emissions and
climate policy to mitigate them remain the major determinant of this risk. Another study estimated that the water vapor will stay in the stratosphere for up to eight years, and influence winter weather in both hemispheres. More recent studies have indicated that the eruption had a slight cooling effect. In September 2023, the Antarctic
ozone hole was one of the largest on record, at 26 million square kilometers. The anomalously large ozone loss may have been a result of the Hunga Tonga–Hunga Haʻapai eruption. == Tsunami ==