'Sea Storms Rattle the Core': Shocking New Study Reveals Ocean Waves Penetrate Deep Into Earth's Interior Layers

Sustainability Times

17-05-2025

IN A NUTSHELL 🌊 Ocean storms in the North Atlantic generate microseisms that travel through the Earth's core, providing new insights into its structure.
in the North Atlantic generate microseisms that travel through the Earth's core, providing new insights into its structure. 🔍 Researchers used spiral-shaped seismometers in Australia to detect PKP waves, a rare type of seismic wave caused by cyclones.
in Australia to detect PKP waves, a rare type of seismic wave caused by cyclones. 🌌 This method could revolutionize planetary exploration by offering a way to study the interiors of planets and moons without tectonic activity.
by offering a way to study the interiors of planets and moons without tectonic activity. ⚙️ Challenges include the faintness of storm-generated signals and the need for advanced equipment and precise data processing techniques.
In a groundbreaking study, scientists have discovered that ocean storms can provide valuable insights into the Earth's interior. Traditionally, researchers relied on earthquakes to study the Earth's core, but this method has proven unreliable. Now, ocean storms, particularly those in the North Atlantic, are offering a more consistent and revealing alternative. As these storms unleash chaos on the ocean's surface, they send shockwaves deep into the Earth, traveling through its liquid outer core and solid inner core. This innovative approach not only enhances our understanding of Earth's structure but also opens new possibilities for exploring other planets. Catching the Sound of the Ocean
When massive storms rage across the North Atlantic, they generate powerful ocean waves that clash, producing tiny vibrations known as microseisms. Unlike vibrations caused by tectonic activity, these microseisms result from storm waves colliding. While their energy is much weaker than that of earthquakes, some of these vibrations can travel thousands of miles through the Earth's core. Previously dismissed as mere background noise, microseisms have now emerged as a treasure trove of data, thanks to advanced equipment and sophisticated processing techniques.
To capture these subtle vibrations, researchers from the Australian National University (ANU) deployed two arrays of spiral-shaped seismometers in remote areas of Queensland and Western Australia. These instruments were specifically designed to detect PKP waves, a rare type of seismic wave generated by cyclones that travel through Earth's core. During Australia's summer months, the team successfully recorded signals produced by winter storms in the far northern Atlantic. Although the strength of these microseisms was only a fraction of that produced by earthquakes, their frequent and uniform occurrence made them ideal for studying the Earth's inner layers.
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While Earth is known for its tectonic activity, many other planetary bodies lack such frequent geological events. However, they do have atmospheres and storms, which could generate similar microseisms. By detecting these vibrations, scientists could gain insights into the interiors of planets without relying on earthquakes. This technique, however, presents certain challenges. The faint storm-generated signals can be easily masked by local noise, and their detection depends on factors such as seafloor topography, ocean depth, and storm characteristics. As a result, not all locations on Earth or other planets are equally suitable for this approach.
According to Hrvoje Tkalčić, a co-author of the study and professor at ANU, the signals are complex and vary based on the source and receiver path. Efficient methods and modern observational infrastructure, such as ocean bottom seismometer pools, are essential for detecting and recording these signals. Future research will focus on refining equipment and studying how seismic waves change as they pass through different parts of Earth's core. The findings of this study have been published in the journal Seismological Research Letters.
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The discovery that ocean storms can reveal information about the Earth's interior has significant implications for planetary exploration. As scientists seek to understand the composition and structure of other planets, this method offers a promising alternative to traditional seismic techniques. By detecting microseisms generated by storms on other planets, researchers can gather data about their internal structures without relying on tectonic activity, which may be absent.
This approach is particularly valuable for exploring icy moons and other celestial bodies where earthquakes are unlikely to occur. Abhay Pandey, a PhD student at ANU and study co-author, emphasizes that this method could be instrumental in identifying planets with cores, even those lacking plate tectonics or volcanic activity. By leveraging weather-driven vibrations, scientists can gain a deeper understanding of our solar system and beyond, paving the way for future exploration missions.
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Despite the exciting potential of using ocean storms to study planetary interiors, several challenges remain. The faintness of storm-generated signals requires advanced equipment and precise data processing techniques. The detection of these signals is influenced by various factors, including the seafloor's shape, ocean depth, and storm intensity. As such, researchers must carefully select study locations to maximize the effectiveness of this approach.
Moving forward, scientists will continue to refine their equipment and methods to enhance the detection and analysis of microseisms. By improving our understanding of how these vibrations interact with Earth's core, researchers can unlock new insights into our planet's structure. Additionally, as we venture into space exploration, this method could become a valuable tool for studying the interiors of other planets and moons. How will this innovative approach shape our understanding of the universe and our place within it?
Our author used artificial intelligence to enhance this article.
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