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首页> 外文期刊>International Journal of Offshore and Polar Engineering >2010 Chilean Tsunami Observed on Japanese Coast by NOWPHAS GPS Buoys, Seabed Wave Gauges and Coastal Tide Gauges
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2010 Chilean Tsunami Observed on Japanese Coast by NOWPHAS GPS Buoys, Seabed Wave Gauges and Coastal Tide Gauges

机译:NOWPHAS GPS浮标,海底波浪仪和沿海潮汐仪在日本海岸观测到的2010年智利海啸

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摘要

The 2010 Chilean Tsunami was observed on the Japanese coast by 11 GPS buoys of NOWPHAS (Nationwide Ocean Wave Information Network for Ports and Harbours); these buoys measured the water level by using real-time kinematic GPS technology at a water depth of 100 to 300 m. The highest tsunami crest was 0.1 to 0.3 m, and the predominant period was longer than 50 min. Owing to the coastal bathymetry, tsunami components longer than 30 min at the GPS buoy sites appeared amplified to nearby seabed wave gauge sites at water depths of 30 to 50 m, and the shorter components of 10 to 20 min appeared significantly amplified at the coastal tide gauge sites.
机译:2010年智利海啸在NOWPHAS(全国港口和港口海浪信息网络)的11个GPS浮标上观测到了日本海岸;这些浮标使用实时运动GPS技术在100至300 m的水深处测量了水位。最高海啸波峰为0.1至0.3 m,主要时段超过50分钟。由于沿海测深,在30到50 m的水深处,GPS浮标处长于30分钟的海啸分量被放大到附近的海床波幅仪地点,而在沿海潮汐中,短于10到20分钟的海啸分量则被明显放大。测量站点。

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