Someone on the NASA Facebook site asked, “Has the Tonga volcano (the name of the volcano is actually Hunga, which erupted off the coast of Tonga) put enough dust into the atmosphere to affect the global average temperature, as Mt. Pinatubo did back in 1991?”

The next day someone at NASA took the time to answer the question,:
“The main climate impacts of volcanic eruptions is not from their carbon dioxide emissions (small compared to that coming from human activities) but from the short-term cooling induced by their sulfur dioxide (SO2 ) aerosols emitted.
The total SO2 mass from the Tonga eruption was 0.4 teragrams — 400 million kilograms — of SO2 , which is well below what could significantly alter global climate.
For instance, the Mount Pinatubo eruption in 1991 released 15 to 20 teragrams (1 teragram represents 1,000,000,000 [1 billion] kilograms) of SO2 high into the atmosphere, resulting in a 0.6 degree Celsius (1 degree Fahrenheit) drop in global temperature over the next 15 months. That amount is 37.5 to 50 times greater the relatively small amount of SO2 emitted from the Tonga eruption.”

The June 12, 1991 eruption column from Mount Pinatubo taken from Clark Air Base.
Date U.S. Geological Survey Photograph taken by Richard P. Hoblitt.
https://earthobservatory.nasa.gov/…/global-effects-of…https://ozoneaq.gsfc.nasa.gov/data/aerosols/…https://so2.gsfc.nasa.gov/pix/daily/0122/tonga_0122z.htmlhttps://so2.gsfc.nasa.gov/
More Details About the Hunga(Tonga)Eruption
- Amplified Explosion. The fact that the volcano is located in relatively shallow water (150 m) led to a bigger explosion. The steam generated from the contact between magma and seawater led to additional gas pressure that could not be offset enough by the overhanging pressure of the seawater at that depth.
- The Shock Wave. “The blast produced a shock wave in the atmosphere that was one of the most extraordinary ever detected, said Corwin Wright, an atmospheric physicist at the University of Bath in England. Satellite readings showed that the wave reached far beyond the stratosphere, as high as 60 miles up, and propagated around the world at more than 600 miles an hour.” (NY Times, Here’s What Scientists Know About the Tonga Eruption, Jan19, 2022″.
- Volcanic Lightning. In the title-picture we notice a beautiful bolt of lightning. This was not caused by a coincidental storm but by the ash itself. The rapidly expanding particles from the ash have enough kinetic energy to cause electrons to move out of the dust, leading to massive static. If the charges are separated in the eruption-cloud there could be enough voltage to cause a discharge.
More Details About Pinatubo and Atmospheric Perturbations from Volcanoes:
- The Pinatubo eruption was the 2nd largest of the 20th century, spewing ash to a height of 40 km, which is in the upper stratosphere, home of the ozone layer.
- The combined effect of volcanic particles and anthropogenic reactive chlorine led to record low levels of stratospheric ozone. (Nature volume 373, pages399–404 (1995))
- How? The particles that the eruption injected into the stratosphere provided sites for heterogeneous chemical reactions, akin to the way polar stratospheric clouds(PSFs) accelerate ozone depletion over Antarctica. The set of reactions lowers reactive nitrogen species, which are needed to act as an important buffer to ozone loss. For example, NO2 is involved in reactions which convert reactive chlorine into non-reactive forms, preventing it from destroying more ozone. But if NO2 is sequestered by either PSFs or volcanic aerosols, then more catalyst(Cl) is available to wreak havoc.
- Pinatubo killed over 800 people, damaged farmlands and thousands of homes. It also caused about $100 million of damage to aircraft.

How Well Do You Know Your Volcanoes?

1B, 2C, 3E, 4A, 5D