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Numerical Modeling and Observations of Tsunami Waves in Alberni Inlet and Barkley Sound, British Columbia

机译:不列颠哥伦比亚省阿尔伯尼湾和巴克利湾海啸波的数值模拟和观测

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Alberni Inlet is a long and narrow fjord adjacent to Barkley Sound on the Pacific Coast of Vancouver Island, Canada. Port Alberni, at the head of the inlet, was affected in 1964 by the largest Pacific tsunami waves in Canadian history. We use observations and results from two numerical models to investigate the resonant characteristics of the region and amplification of tsunami waves in Barkley Sound and Alberni Inlet. The first model (A) was forced at its open boundary with a stationary autoregressive signal, similar to the observed background noise. The second model (B) used an initial sea-level deformation from a potential earthquake off California in the southern segment of the Cascadia Subduction Zone, producing transient tsunami waves. Spectral, cross-spectral and frequency-time (f-t) analyses of the observations were used to examine the resonant properties and topographic response of the local area. The respective results show large admittance functions over a wide 0.5-0.9 cph frequency band, implying a low Q factor but high amplification of arriving waves. This unusual behavior is a result of two effects: A quarter-wave resonance of the system for its fundamental Helmholtz mode and amplification due to the narrowing of the channel cross section from Barkley Sound to Alberni Inlet. The model A numerical results agree favorably with the observations, indicating an energetic resonant mode at frequency of similar to 0.53 cph (112 min), with its nodal line located near the entrance to Barkley Sound and amplification factor value close to 12. The results from the tsunami propagation model (B) yield spectral characteristics similar to those from the model A and from the observations. The maximum tsunami current speed for this scenario is 2.4 ms(-1) in Sproat Narrows, which divides Alberni Inlet into two parts, while the largest computed wave height is 1.6 m in the northern Alberni Inlet, in the area of Port Alberni.
机译:Alberni Inlet是一条细长的峡湾,毗邻加拿大温哥华岛太平洋海岸的Barkley Sound。 1964年,加拿大北部最大的太平洋海啸波影响了阿尔伯尼港(Alberni港)的入口。我们使用来自两个数值模型的观测结果来调查该区域的共振特征以及海啸在Barkley Sound和Alberni Inlet中的放大。第一个模型(A)用一个固定的自回归信号强迫其开放边界,类似于观察到的背景噪声。第二个模型(B)使用了卡斯卡迪亚俯冲带南部段加利福尼亚附近的一次潜在地震引起的初始海平面变形,产生了短暂的海啸波。观测的光谱,互谱和频率-时间(f-t)分析用于检查局部区域的共振特性和地形响应。各自的结果表明在0.5-0.9 cph的宽频带上具有大的导纳函数,这意味着低Q因子但对到达波的放大很高。这种不正常的行为是由于以下两种效应造成的:系统的基本亥姆霍兹模式发生了四分之一波长谐振,并且由于从Barkley Sound到Alberni Inlet的通道横截面变窄而放大。模型A的数值结果与观测值吻合良好,表明能量共振模式的频率接近0.53 cph(112分钟),其节点线位于Barkley Sound入口附近,放大系数值接近12。海啸传播模型(B)产生的光谱特征类似于模型A和观察到的光谱特征。在Sproat Narrows中,这种情况下的最大海啸当前速度为2.4 ms(-1),它将Alberni Inlet分为两部分,而在Alberni Port北部地区,最大的计算波高在Alberni Inlet北部为1.6 m。

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