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Relationship Between Maximum Tsunami Amplitude and Duration of Signal

机译:海啸最大振幅与信号持续时间的关系

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All available tsunami observations at tide gauges situated along the North American coast were examined to determine if there is any clear relationship between maximum amplitude and signal duration. In total, 89 historical tsunami recordings generated by 13 major earthquakes between 1952 and 2011 were investigated. Tidal variations were filtered out of the signal and the duration between the arrival time and the time at which the signals drops and stays below 0.3 m amplitude was computed. The processed tsunami time series were evaluated and a linear leastsquares fit with a 95 % confidence interval was examined to compare tsunami durations with maximum tsunami amplitude in the study region. The confidence interval is roughly 20 h over the range of maximum tsunami amplitudes in which we are interested. This relatively large confidence interval likely results from variations in local resonance effects, late-arriving reflections, and other effects.
机译:检查了沿北美海岸的潮汐仪上所有可用的海啸观测值,以确定最大振幅与信号持续时间之间是否存在明确的关系。总共调查了1952年至2011年间13次大地震产生的89次历史海啸记录。从信号中过滤出潮汐变化,并计算到达时间与信号下降并保持在0.3 m振幅以下之间的持续时间。评估了处理过的海啸时间序列,并检查了具有95%置信区间的线性最小二乘拟合,以比较研究区域的海啸持续时间与最大海啸振幅。在我们感兴趣的最大海啸振幅范围内,置信区间大约为20小时。此相对较大的置信区间可能是由于局部共振效应,迟到反射和其他效应的变化而引起的。

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