Hurtling towards the earth 30 times faster than a rifle bullet, a 1,400-ton fireball exploded with the energy of 10 Hiroshima bombs in a blinding flash on the night of Dec 18, 2018, becoming the third largest meteor impact in modern times.
However, the explosion, 15.5 miles above the remote Bering sea, had no witnesses and was picked up only on NASA instruments, which had held onto their secret until now.
The data was picked up by infrasound stations globally which were initially set up to detect nuclear blasts during the cold war.
According to Brown, the data was gathered from 16 infrasound stations worldwide.
It is unclear why the data was released so late.
According to the New Scientist the triangulation process requires combining pressure wave data from multiple monitoring stations, which could explain the delay.
It is the third-largest such explosion recorded in over a century, and the largest since the Chelyabinsk meteor six years ago.
“That’s another thing we have in our defense, there’s plenty of water on the planet,” she said.
The explosion over the Bering Sea was also picked up by U.S. government monitors that detect fireballs: their sensors pick up electromagnetic radiation in the form of infrared and visible light.
But both the Bering Sea and Chelyabinsk explosions are smaller than the earliest well-documented meteor explosion known as the Tunguska event, which occurred over Siberia in 1908. That air burst explosion from the 220 million pound rock, about 120 feet wide, flattened an estimated 80 million trees over an area of more than 770 square miles.
“Ann Hodges of Sylacauga, Alabama, was severely bruised by a 8-pound (3.6-kilogram) stony meteorite that crashed through her roof in November 1954,” NASA’s website states.
For scientists who know where to look, the earth is pockmarked with evidence of large impacts.
“One of the most intact impact craters is the Barringer Meteor Crater in Arizona,” according to the NASA website. “It’s about 0.6 miles (1 kilometer) across and was formed by the impact of a piece of iron-nickel metal approximately 164 feet (50 meters) in diameter. It is only 50,000 years old and so well preserved that it has been used to study impact processes. Since the 1890s geologists studied it, but its status as an impact crater wasn’t confirmed until 1960.”