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THE MYSTERY OF 2010 CHILEAN EARTHQUAKE GENERATED TSUNAMI WAVES AT CRESCENT CITY HARBOR

机译:2010年智利地震的神秘发电在新月城港口的海啸

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The tsunami generated by the 2010 Chilean earthquake was recorded at several tide gauge stations along the Pacific coast from 02/27/2010 to 03/02/2010. The marigram at the tide gauge station in Crescent City Harbor in Northern California is analyzed in detail because Crescent City is well known for its tsunami vulnerability. The energy spectrum as a function of frequency has been found to contain several spikes corresponding to the frequency range of 3×10~(-4) ~8×10~(-4) Hz . This behavior is different from several prior tsunamis observed and analyzed for Crescent City Harbor. A finite element numerical model has been used to compute the resonant response at Crescent City Harbor to incident waves with different wave directions. It is found that the spectral spikes are associated with the first fundamental mode of oscillation at the dimensionless wave number kl = 1.10 for different water depth due to the varying tide levels (0.6 to 3.9 meters). A closer view of the spectral density curves found that everyday tide gauge record also contained the same multi-spectral-spikes because of the significant variation of water depth from low tide to high tide. In order to correctly decipher the resonant response characteristics to incident wave the response curve plotted as a function of the dimensionless wave number is essential.
机译:2010年智利地震产生的海啸在太平洋沿岸的几个潮汐量站记录在太平洋海岸,从02/27/27/2010-021010记录。在加利福尼亚州北加州新月城港口的Tide Caudge站的Marigram进行了详细分析,因为新月城以其海啸脆弱而闻名。已经发现作为频率函数的能谱含有几个对应于3×10〜(-4)〜8×10〜(-4)Hz的频率范围的尖峰。这种行为不同于几个先前的海啸观察和分析了新月城港口。有限元数值模型已用于计算新月城港口的共振响应与不同波方向的入射波。结果发现,由于不同的潮水平(0.6〜3.9米),光谱穗在无量纲波数KL = 1.10处与不同的水深度的第一基本振荡模式相关联。较近的光谱密度曲线的视图发现,日常潮仪记录还包含相同的多光谱 - 尖峰,因为水深从潮汐到高潮中的水深变化。为了正确地破译反应的谐振响应特性,进入波的响应曲线作为无量纲波数的函数绘制的曲线是必不可少的。

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