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Both waveforms observed in the Coral Sea show the wave dispersion, with a shorter period wave following the long period wave.
In this paper, a physical modeling experiment of sediment under long period wave is carried out.
For the 50-year return period wave heights, the EST estimated larger values than the LSM by 2%26%%.
Numerical results demonstrate the significant effects of current in case of larger water depth, smaller period wave and fine sand.
Finally, in mesospheric winter, the periods of the extra-long period wave band are weaker compared to the nSV-simulation.
Moreover, in mid-latitudes such 27-day oscillations can be the dominant period of the extra-long period wave band.
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Overtopping is particularly sensitive to these longer period waves, potentially resulting in coastal flooding.
This feature increases the dynamic response of the structure on short period waves (springing) and on impulsive wave loads (whipping).
Both long period and shorter period waves are communicated via the dedicated webpage (http://www.tsunamigps.com/gpsreal.php).php
However, historical experience shows occasional severe impacts from long period waves, such as on 6th February 1904, 13th February 1979 and most recently two events in February 2014.
Example of 630.0 nm images processed using length-8 FIR filters with passbands of (left) 0.3 to 1.7 mHz, (middle) 0.3 to 1.0 mHz to highlight the 26.2-min period waves, and (right) 1.0 to 1.7 mHz to highlight the 14.2-min period waves.
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