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- W2090004211 abstract "A WERA phased array HF radar was used in Chile to observe the disturbance of the 11 March 2011 tsunami which originated near Japan. In this pilot study, three sites on a transect across the shelf were analysed at water depths of 40, 160 and 880m. The maximum wave orbital velocities increased as the wave-group propagated into shallow water. The increase in maximum wave orbital velocities between 160 m depth and 40 m depth followed linear theory, but between 880 m and 160 m depths, the tsunami wave-group was non-linear and over half the amplitude was lost. The HF radar data indicate that non-linear processes are occurring at this location as the tsunami disturbance propagates from deep water onto the continental shelf." @default.
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- W2090004211 date "2014-09-01" @default.
- W2090004211 modified "2023-10-14" @default.
- W2090004211 title "Observations and theory of a shoaling tsunami wave" @default.
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- W2090004211 doi "https://doi.org/10.1109/oceans.2014.7003236" @default.
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