As one of Japan’s most active volcanoes, Sakurajima often dazzles with spectacular displays of volcanic lightning set against an ash-filled sky. But the volcano can also produce much smaller, invisible bursts of electrical activity that mystify and intrigue scientists.
Now, an analysis of 97 explosions at Sakurajima from June 2015 is helping to show when eruptions produce visible lightning strokes versus when they produce the mysterious, unseen surges of electrical activity, reported researchers recently.
These invisible bursts, called vent discharges, happen early in eruptions, which could allow scientists to figure out ways to use them to warn of impending explosions.
Volcanic lightning formation
Researchers know that volcanic lightning can form by silicate charging, which happens both when rocks break apart during an eruption and when rocks and other material flung from the volcano jostle each other in the turbulent plume.
Tiny ash particles rub together, gaining and losing electrons, which creates positive and negative charges that tend to clump together in pockets of like charge. To neutralize this unstable electrical field, lightning zigzags between the charged clusters.
Experiments have shown that you can’t get lightning without some amount of ash in the system. “So if you’re seeing volcanic lightning, you can be pretty confident in saying that the eruption has ash.”
Vent discharge formation
Vent discharges, on the other hand, are relatively newly detected bursts of electrical activity, which produce a continuous, high-frequency signal for seconds — an eternity compared with lightning. These discharges can be measured using specialized equipment.
By focusing on small explosions from Sakurajima, defined as those with plume heights of 3 kilometers or less and with a duration of less than five minutes, Smith and colleagues examined silicate charging, plume dynamics and the relationship between volcanic lightning and vent discharges.
As expected, the team found that lightning at Sakurajima occurred in plumes replete with ash. Vent discharges, however, occurred only when ash-rich plumes with volcanic lightning rocketed skyward at velocities greater than about 55 kilometers per second.
“Once you get to a certain intensity of eruption,” Smith says, “you’re going to see these vent discharges.”
Monitoring vent discharges
Monitoring these discharges could be especially helpful for quickly spotting eruptions that have a lot of ash in them. Tracking ash is vital because that’s what’s dangerous for aviation and local communities in many instances.
Electrical activity signals an ash-rich plume no matter the weather or time of day, and vent discharges provide a measure of an eruption’s intensity, which could help observatories model where a plume might go.
Vent discharges to provide early warnings
Tracking lightning and vent discharges could cover gaps left by other ways of monitoring volcanoes.
Seismologists track underground movements of magma to look for signs of an impending eruption. Infrasound is used to indicate when an explosion has occurred, but the technique doesn’t differentiate between ash versus gas in eruptions. And satellites collect data on eruptions, though in many cases that’s dependent on good weather at the right time.
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