North Korea blast lights up �Ӱ�ԭ�� seismometers

September 7, 2017

Graphic by Helena Buurman, �Ӱ�ԭ�� Earthquake Center.. Twenty red triangles across the map of �Ӱ�ԭ��, at lower left, correspond with seismometer recordings, at right, of an underground nuclear bomb detonation Sept. 2, 2017, in North Korea, at the center of the map in the upper left. The energy reached �Ӱ�ԭ�� just after 7:30 p.m. that day.

On Saturday night, Sept. 2, Matt Gardine was at home outside Fairbanks playing with his daughter when his phone beeped. As the seismologist on call with the �Ӱ�ԭ�� Earthquake Center, Gardine’s duty was to get information out about detectable earthquakes right after they happen.

A few minutes earlier, at 7:30 p.m., a wave of energy had passed through �Ӱ�ԭ��. The shake had propagated through the entire planet, first reaching �Ӱ�ԭ�� near the village of Wales and racing southeast from there.

Looking at the waveform that registered on seismometers from Tin City to Ketchikan, Gardine noticed its squiggle signature did not look like an earthquake. He saw its origin was North Korea, which doesn’t have many large earthquakes. He also thought it curious that the disturbance occurred right on the half hour, at 7:30.

Though people in China and Russia reported feeling a shake, which U.S. Geological Survey scientists estimated as magnitude 6.3 at its source in North Korea, Gardine suspected no �Ӱ�ԭ��ns would detect the movement and that it was not an earthquake. He issued no alerts.

The shake that registered on �Ӱ�ԭ�� seismometers and most sensitive instruments worldwide was an underground nuclear explosion by North Koreans. Since the Comprehensive Nuclear-Test-Ban Treaty in 1996, North Korea has been the only country conducting these tests.

“It was almost certainly underground,” Gardine said. “They did it to test that they can detonate a bomb, that their bombs are good.”

Detecting nuclear explosions is not the job of the researchers who work at the �Ӱ�ԭ�� Earthquake Center, based at the university in Fairbanks. There is an Air Force agency, the Technical Applications Center, with that responsibility.

But Mike West, �Ӱ�ԭ��'s state seismologist, said he and others at the center are “scientifically deeply interested” in the blasts. More than 400 seismometers planted around �Ӱ�ԭ�� have registered two North Korea tests last year and one in 2015. Seismometers all over North America caught the same signals a few minutes later.

Underground explosions register with more clarity than earthquakes, West said. The recent burst was also followed by a second, smaller energy spike that was one of the reasons West invited all scientists to a post-Labor Day gathering to discuss the blast. The second signal was the energy of the nuclear bomb bouncing off the outer core of the Earth and returning to seismometers.

The North Korean bomb was a small blast compared to one in �Ӱ�ԭ�� on Nov. 6, 1971. That’s when U.S. Atomic Energy Commission officials executed the largest underground nuclear test ever done in America. That 5-megaton bomb, named project Cannikin, was detonated in a shaft more than one mile deep beneath Amchitka Island in the western Aleutians.

Since the late 1970s, the University of �Ӱ�ԭ�� Fairbanks' Geophysical Institute has provided this column free in cooperation with the UAF research community. Ned Rozell is a science writer for the Geophysical Institute.