The Meteorological Research Institute reproduced wave movements with a supercomputer, using data on water pressure captured in the seabed observation network off the Tohoku region.
The analysis showed that the tsunami initially travelled across the Pacific Ocean and reached the coast of South America, about 15,000km away from the quake’s epicentre.
The waves then bounced off the coast and travelled back towards Japan via the Pacific.
The rebound tsunami waves are projected to have reached Japan about 48 hours after the earthquake, when tsunami warnings and advisories had been lifted.
In fact, 0.6m-high waves were observed in Kamisu, Ibaraki prefecture, and Kuji, Iwate prefecture, in the morning of August 1.
The agency found that the tsunami could not be reproduced in an analysis that assumed there was no South American continent, only ocean.
Tsunami advisories are issued when waves are projected to be at least 0.2m high and are expected to cause damage.
“At that time, the public was fully aware that [the] tsunami had been observed. As we concluded that there was no risk of damage, we did not issue another advisory,” a Meteorological Agency official said.
In 1960, a tsunami caused by a magnitude 9.5 earthquake off the coast of Chile reached Japan in about 22 hours and left more than 100 people dead or missing.
“Tsunami can arrive far later than the first tsunami waves,” said Hiroaki Tsushima, a chief researcher at the Meteorological Research Institute.
“The public should be more aware when it comes to disasters and be prepared for a similar earthquake.”
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