
The SWOT satellite, a joint effort by NASA and the French space agency, has provided the first high-resolution observations of a tsunami forming after an earthquake struck off the coast of Kamchatka. This data will empower scientists to enhance predictions of hazardous natural events and ultimately save lives.
In a historical first, the SWOT satellite captured the precise moment a tsunami began to form following a powerful earthquake near the Kamchatka Peninsula. As reported by Naked Science, the information gathered from orbit grants researchers entirely new capabilities for studying and forecasting dangerous oceanic phenomena.
Last July, an earthquake with a magnitude of 8.8 occurred within a subduction zone beneath the Pacific Ocean. Decades of built-up tension were released in mere seconds, causing the seafloor and the overlying water mass to shift. This displacement generated a massive wave that propagated across the ocean at aircraft speeds, eventually hitting coastlines with heights exceeding 17 meters.
Previously, tracking the genesis of a tsunami in its initial location with detail was extremely difficult, primarily due to a scarcity of sensors near deep-sea trenches. Conventional monitoring systems rely on DART buoys, which register pressure changes on the seabed. However, these buoys only provide readings from discrete points and fail to capture the overall structure of the wave.
This situation has changed thanks to the Surface Water and Ocean Topography (SWOT) satellite, a collaboration between the US and French space agencies. Seventy minutes after the earthquake, the spacecraft traversed the Pacific, located 600 km from the epicenter, and recorded not only the leading edge of the wave but also a train of smaller, trailing disturbances—dispersion waves—in high fidelity.
A research team led by Ignacio Sepulveda from the University of California San Diego analyzed the satellite readings. Initially, the researchers attempted to simulate the event using a standard shallow-water model, which failed to replicate all the observed characteristics. Consequently, the team shifted to a more complex Boussinesq-type model, which successfully accounted for their observations.
“Thanks to the satellite data, we can model extreme oceanic events with greater accuracy and potentially improve our forecasts in the future,” the scientists noted.
As a result of this analysis, specialists could pinpoint the tsunami generation area to within 10 km of the deep-sea trench—a first in scientific history. This breakthrough paves the way for superior prediction capabilities. It now allows for more precise calculations of wave height, arrival time, and impact force upon coastal areas. In the long term, such technology promises faster warning issuance, more effective evacuation coordination, and the preservation of human lives during future major tsunamis.