The big swells invade the Toyama Bay from October to March as usual, and cause wave disasters repeatedly since long ago on the coast of Toyama bay. Furthermore, LNG cargo handling is carried out regularly in Toyama New Port, and it is dangerous because, swells invaded the port give bad influence to the cargo handling. Therefore, it is important to investigate swells invaded the port. And so, we investigated swells in the Toyama New Port by the comparison of swells off and in the port. Summaries of obtained results are as follows.
(1)The shapes of wave spectra in the port are different from those off the port.
(2)The shapes of wave spectra in the port are almost the same, independently of shapes of wave spectra off the port.
(3)Attenuation rates of swells with about 14 second, about 13 second and about 11 second period, which invaded Toyama New Port, are smaller than those of swells with other periods which invaded the port.
It was shown that wave height of long period wave with about 30 minute period, which invaded Toyama New Port, increases four times compared to the wave height before invading the port in another study. Furthermore, it was shown that attenuation rates of swells, which invaded the port, are different depending on those wave periods in this paper. The authors consider that the cause that the attenuation rates of swells are different depending on the wave periods, is that wave heights of swells with particular periods which invaded the port, increase at the end of the port. It is a future problem to make clear the generating mechanism of those phenomena.
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