The planet Earth is a world flourishing with all kinds of life that is the result of billions of years of geologic processes that we still don’t understand, and likely never will. While it’s easy to study everything above ground, learning about the interior of our small, blue world is quite impossible to observe directly, for the simple reason that we literally can’t venture down into the depths of the planet itself. Therefore, scientists must rely on seismic waves to study the interior of the Earth, which has taught us quite a bit about how the Earth’s interior.
In a recent study published in Science Advances, USC scientists have found evidence that the Earth's inner core oscillates, contradicting previously accepted models that suggested it consistently rotates at a faster rate than the planet's surface.
Their study shows that the inner core changed direction in the six-year period from 1969-74, according to the analysis of seismic data. The scientists say their model of inner core movement also explains the variation in the length of day, which has been shown to oscillate persistently for the past several decades.
"From our findings, we can see the Earth's surface shifts compared to its inner core, as people have asserted for 20 years," said John E. Vidale, co-author of the study and Dean's Professor of Earth Sciences at USC Dornsife College of Letters, Arts and Sciences. "However, our latest observations show that the inner core spun slightly slower from 1969-71 and then moved the other direction from 1971-74. We also note that the length of day grew and shrank as would be predicted. The coincidence of those two observations makes oscillation the likely interpretation."
Utilizing data from the Large Aperture Seismic Array (LASA), a U.S. Air Force facility in Montana, researcher Wei Wang and Vidale found the inner core rotated slower than previously predicted, approximately 0.1 degrees per year. The study analyzed waves generated from Soviet underground nuclear bomb tests from 1971-74 in the Arctic archipelago Novaya Zemlya using a novel beamforming technique developed by Vidale.
The new findings emerged when Wang and Vidale applied the same methodology to a pair of earlier atomic tests beneath Amchitka Island at the tip of the Alaskan archipelago -- Milrow in 1969 and Cannikin in 1971. Measuring the compressional waves resulting from the nuclear explosions, they discovered the inner core had reversed direction, sub-rotating at least a tenth of a degree per year.
This latest study marked the first time the well-known six-year oscillation had been indicated through direct seismological observation.
"The inner core is not fixed -- it's moving under our feet, and it seems to going back and forth a couple of kilometers every six years," Vidale said. "One of the questions we tried to answer is, does the inner core progressively move or is it mostly locked compared to everything else in the long term? We're trying to understand how the inner core formed and how it moves over time -- this is an important step in better understanding this process."
As always, keep doing science & keep looking up!