Deep Ocean Floor Can Focus Tsunami Waves
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An image from an animation of the devastating magnitude 9.0 earthquake that rocked Japan in March. CREDIT: NASA/Jesse Allen, using data provided by Tony Song (NASA/JPL) |
Researchers from NASA's Jet Propulsion Laboratory and Ohio State University used satellite altimeters, which can measure sea level changes in very fine detail, to observe "merging tsunamis" — a phenomenon where smaller waves merge to form one bigger wave. These waves can travel hundreds to thousands of miles without losing power.
The measurements showed that the March 2011 tsunami doubled in intensity when passing over rugged ocean ridges and around islands in the middle of the Pacific.
The team used a computer-based model to translate the measurements into images and animations, which shows how the waves can refract, bend and merge as they propagate. The peaks of waves are colored red-brown, while depressions in sea surface appear blue-green. Grayscale outlines show the location of mid-ocean ridges, peaks and islands.
"It was a one in 10 million chance that we were able to observe this double wave with satellites," said Tony Song, principal investigator of the study and a scientist at JPL.
"Researchers have suspected for decades that such ‘merging tsunamis’ might have been responsible for the 1960 Chilean tsunami that killed about 200 people in Japan and Hawaii, but nobody had definitively observed a merging tsunami until now. It was like looking for a ghost," Song said. "Jason happened to be in the right place at the right time to capture the double wave."
