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A "weather bomb" is a storm over the ocean with intense central pressure, producing strong winds and ocean swell that result in some wave-generated seismic activity.
Small, intense storms known as "weather bombs" may trigger rare tremors deep within the Earth, offering scientists a new way to study the mysterious structure and inner workings of the planet, according to a new study.
A "weather bomb" is an extratropical (outside of the tropical zone) storm in which the central pressure intensifies rapidly. These storms produce very strong winds that cause the ocean to swell, generating powerful waves. Some of the wave energy from these storms interacts with the seafloor, causing wave-generated seismic activity.
However, observations and analysis of microseismic activity have focused mostly on P waves — the first set of waves in an earthquake that deliver a sharp jolt — because of their larger amplitudes. This gives scientists only a narrow view of the Earth's structure, because P waves typically travel in straight lines.
The faint and deep tremors "weather bombs" can cause in the oceanic crust run through the earth and can be detected in places as far away as Japan.
(Image credit: Kiwamu Nishida and Ryota Takagi)
In their new study, the scientists detected so-called S wave microseisms, which travel much more slowly and curve through the ground but are generally more difficult to observe. The previously unobserved S waves were generated under a weather bomb between Greenland and Iceland in December 2014.
The researchers detected both P-wave and S-wave microseisms triggered by the severe North Atlantic storm at their station in Japan. In their paper, the authors described the direction and distance to the waves' origins.
Mapping the microseisms provides insight into the planet's deep structure. As seismic energy from the weather-bomb storm travels through the deep Earth, the planet's interior structure is revealed, the researchers said. This is especially beneficial in areas where such monitoring is limited — such as the oceans.
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"We would like to explore the Earth's interior beneath the storm in oceanic areas, where no earthquakes and no stations exist," study co-author Kiwamu Nishida, a professor at the Earthquake Research Institute at the University of Tokyo, told Live Science.
With more acute observations of these storms and the microseisms they cause, scientists can better understand the Earth's internal structure. And understanding the precise locations of P waves and S waves and how they move can also help scientists learn how the seismicity occurs, the researchers explained in their paper.
"Delineation of the source locations and energy partition of the seismic wave components are key to understanding the excitation mechanisms," the authors wrote. As such, the findings could contribute to more accurate detection of earthquakes and oceanic storms.
The new study was published online today (Aug. 25) in the journal Science.
Kacey Deamer is a journalist for Live Science, covering planet earth and innovation. She has previously reported for Mother Jones, the Reporter's Committee for Freedom of the Press, Neon Tommy and more. After completing her undergraduate degree in journalism and environmental studies at Ithaca College, Kacey pursued her master's in Specialized Journalism: Climate Change at USC Annenberg. Follow Kacey on Twitter.
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