The Search for What Shook the Earth for Nine Days Straight

The Search for What Shook the Earth for Nine Days Straight

Introduction

Megatsunamis usually form when a large, swiftly moving mass plunges into a constricted body of water. The combination of extremely high waves and fast speeds has enormous destructive potential.

As this one careened through a section of the 35-kilometer-long fjord, it stripped away Inuit archaeological sites and 20th-century trapper hunts. It escaped into the sea and partially inundated a scientific and military outpost 72 kilometers away on Ella Island, where its (now far smaller) waves caused $200,000 in damages. Thankfully, nobody was injured or killed.

The initial landslide and the ensuing rock-ice avalanche made a lot of noise. Its acoustic roar was picked up more than 3,300 kilometers away, in Russia, by an infrasound instrument designed to detect clandestine nuclear weapons tests. Seismometers also picked up a salvo of high-frequency seismic events, along with some low-frequency waves that came from the acceleration and deceleration of the mass grinding on the Earth’s surface.

What came next wasn’t quite so straightforward.

Seismologists picked up a deep hum oscillating at 10.88 millihertz. “This thing was showing up like a really big anomaly, sticking out like a sore thumb,” Hicks said. As they watched it persist for a day, then another, then another, researchers across the world were stunned. “What’s going on here? Why are we still seeing this?” he said, summing up the shock at the time.

By the time the hum had decayed after nine strange days, a variety of experts, from tsunami researchers to deep-Earth geoscientists, had gathered into an expansive chat group on an open-source platform called Mattermost. They debated all sorts of possible explanations, from the routine to the avant-garde.

The seismic signals didn’t match the signature of an earthquake. Perhaps an ice sheet, disturbed by the rockfall, was ringing like a bell. Maybe the landslide had forced a chunk of ice to melt, and that water slipped through a natural piping system in a glacier, turning it into an instrument and creating the geological equivalent of music. Or could the Greenlandic hum be the work of some incognito volcanism?

No evidence to support any of these ideas was forthcoming. People started jokingly wondering if it was aliens or dragons having a rave or a tantrum. Some sort of leviathan “always comes up” when abnormalities like this baffle seismologists, Hicks said.

Three days after the great collapse, the Danish navy surveyed the fjord to chronicle the changed landscape. To those scouts, everything seemed tranquil. “It still blows my mind that we’re still seeing this seismic signal going round the world, being produced at that time that they sailed there, and they didn’t notice any discernible disturbance,” Hicks said.

Slosh Party

Despite a dearth of conclusive evidence, one hypothesis stuck around. Perhaps the avalanche created a standing wave that was sloshing back and forth in the fjord. Such a wave, called a seiche, is common in lakes and harbors, although it typically takes shape in the presence of strong winds.

Then, just three weeks after September’s dramatics, a second (weaker) seismic signal emerged from the fjord and spread through the planet. It also appeared to have been trigged by a landslide, and it was accompanied by a smaller tsunami. Checking through historical seismic records going back to the early 1980s, the team soon found four similar events. If those signals were from seiches, then perhaps September’s grumble was too.

But there was a glaring problem with the seiche hypothesis. The avalanche and tsunami were large and forceful, but ephemeral. It wasn’t clear how they could generate or sustain a nine-day seiche.

In desperation, one member of the team tried to re-create the prolonged sloshing in their own bathtub. Alas, Dickson Fjord isn’t straight and symmetrical, so a bathtub made for a poor stand-in. The noble experiment didn’t work.

The team then tried to model the event on a computer. In their first attempts at building numerical simulations of the tsunami, they couldn’t reconstruct the seiche. Then the Danish military gave them access to high-resolution sonar surveys of the fjord’s baroque bottom. That’s when the evidence started to pile up.

Simulations that took into account the varying depth of the fjord showed that the megatsunami had stabilized into a seiche with a dominant frequency of 11.45 millihertz — very close to the 10.88 millihertz frequency of the weird hum. The virtual seiche’s nine-day decay matched that of the real thing. The wonky geography of the fjord suggested that the seiche’s energy would only leak out into open waters gradually, helping to explain its longevity.

Their simulations also revealed the reason the Danish navy failed to see the seiche’s waves in person. The seiche was sloshing the 2.7 kilometers from one side of the fjord to the other every 45 seconds. After just three days, the wave height had decayed to just a handful of centimeters, making it all but imperceptible to anyone present.

The study underscores that our rapidly warming world can affect us in surprising ways. The landslide that kicked off that megatsunami was triggered by a melting film of ice. “Climate change is lurking in the background of this story,” Svennevig said. Researchers will now be on the alert for similar warning signs in other glaciated parts of the planet vulnerable to megatsunamis.

Nine days of global quivering may be impressive, but it’s not a record. The devastating magnitude-9.1 Sumatra-Andaman earthquake and tsunami in December 2004 shook the planet for 18 days. And it’s thought that the Chicxulub asteroid, which ended the reign of the dinosaurs 66 million years ago, rumbled Earth for months after impact.

The difference with the Greenlandic pandemonium is that, luckily, it caused minimal damage and zero casualties. Instead, Earth presented scientists with a riddle — and they went all-in to solve it, simply to satiate their curiosity. “It’s just cool to say: I see a weird signal — what is it?” said Jackie Caplan-Auerbach, a seismologist and geophysicist at Western Washington University who was not involved with the new study. Sometimes, Hicks said, “this kind of science is the most fun.”