In a study, scientists at the University of Utah report as a record of wave motion in a lake. They can reveal when a lake freezes over and when it melts. And as a small, constant source of seismic energy in the surrounding earth. Lake microseisms can shine a light on the geology surrounding a lake.
Seismologists have long known that wind-driven ocean waves generate small seismic waves, called microseisms. These microseisms generated as waves drag across the ocean floor or interact with each other. They are part of the background seismic noise in coastal areas.
“It’s kind of a new phenomenon,” says Keith Koper, director of the University of Utah Seismograph Stations and co-author of the study. “We don’t really know how it’s created.”
“We’ve recently found that the waves on lakes actually generate these microseisms too,” Koper says. Lake microseisms had previously recorded near the Great Lakes, Canada’s Great Slave Lake and Utah’s own Great Salt Lake. Koper and colleagues present additional observations from Yellowstone Lake and three lakes in China, exploring the characteristics of the respective lakes’ microseisms.
Koper says the tremors are very small. “You wouldn’t be able to feel them, that’s for sure,” he says. But by averaging seismic signals over a long period six months, for example a consistent signal emerges.
CT scan of the Earth
The signal can used to produce what Koper calls a “CT scan of the Earth,” or seismic tomography. Seismic waves travel through different geological materials at different speeds, so observing how waves change as they emanate from a source can reveal subsurface geology.
Researchers can create these seismic sources with methods like a hammer on a metal plate, an explosion, or a specially outfitted truck with a vibrating plate. Lakes, Koper says, provide a natural, regular source. “It would take quite a bit of effort and work to generate this level of energy.”
The area that explored using lake microseisms limited to the region close to lake. But Koper writes that lake microseisms emanating from the Great Salt Lake might reach far enough to visualize how seismic waves would move beneath Salt Lake City, which sits on the Wasatch Fault, in a major earthquake. Likewise, Lake Tahoe microseisms could extend to Reno, Nevada, and Lake Michigan could provide microseisms to image the geology beneath the Chicago area.
Microseisms can perform another function, says Aini Mokhdhari, a senior majoring in geology. Because tremors caused by wind-driven waves. Microseisms cease during lake freezes over in winter. They resume again when it thaws in the spring. Thus, rather than relying on satellite or eyewitness observations, lake freezing and thawing monitored by an autonomous seismometer.
Mokhdhari observed at microseismic data from Yellowstone Lake. A well-observed lake for obtaining the freezing and thawing dates. “We compare the data we got from the seismograph to see if it’s the same,” she says. “So far it is.” Seismological observations not needed at Yellowstone Lake. But could be useful for monitoring more remote lakes for long-term changes to ice cover duration.
Next summer, Mokhdhari and Koper will join colleagues in a further seismic study of Yellowstone Lake. They’ll place an array of small seismometers called geophones around the perimeter of the lake, and also place an array of special waterproof seismometers on the lake floor. Additionally, they will use a buoy on the lake to measure wind and wave conditions. Their colleagues are looking to understand the hydrothermal vents in Yellowstone Lake. But Mokhdhari and Koper much more interested in capturing microseisms from all angles.
” In case we record at the same time on land and underwater,” Koper says, “we can get a better idea of how these things are generated.”