论文标题
使用原始波形数据和卷积神经网络快速预测地震地面震动强度
Rapid Prediction of Earthquake Ground Shaking Intensity Using Raw Waveform Data and a Convolutional Neural Network
论文作者
论文摘要
这项研究描述了一种基于深卷卷神经网络(CNN)的技术,用于预测地面震动的强度测量(IMS)。 CNN模型的输入数据由2016年中央意大利地震序列中记录的多稳定宽带和加速度计,以M $ \ ge $ 3.0。我们发现,CNN能够准确地预测远离震中的站点的IMS,并且在使用10 S窗口开始在地震起源时间开始时尚未记录最大的地面摇动。 CNN IM预测不需要以前了解地震来源(位置和幅度)。 CNN模型预测与Bindi等人获得的预测之间的比较。 (2011)GMPE(需要位置和幅度)表明,CNN模型具有相似的误差方差,但偏差较小。尽管该技术并非严格设计用于地震预警,但我们发现它可以根据各种设置元素(例如,用于数据传输,计算,潜伏期)提供15-20秒内地面运动的有用估计。该技术已在原始数据上进行了测试,而无需任何初始数据预选,以便密切复制实时数据流。当地震数据中包括噪声示例时,发现CNN稳定,可以准确预测与噪声振幅相对应的地面摇动强度。
This study describes a deep convolutional neural network (CNN) based technique for the prediction of intensity measurements (IMs) of ground shaking. The input data to the CNN model consists of multistation 3C broadband and accelerometric waveforms recorded during the 2016 Central Italy earthquake sequence for M $\ge$ 3.0. We find that the CNN is capable of predicting accurately the IMs at stations far from the epicenter and that have not yet recorded the maximum ground shaking when using a 10 s window starting at the earthquake origin time. The CNN IM predictions do not require previous knowledge of the earthquake source (location and magnitude). Comparison between the CNN model predictions and the predictions obtained with Bindi et al. (2011) GMPE (which require location and magnitude) has shown that the CNN model features similar error variance but smaller bias. Although the technique is not strictly designed for earthquake early warning, we found that it can provide useful estimates of ground motions within 15-20 sec after earthquake origin time depending on various setup elements (e.g., times for data transmission, computation, latencies). The technique has been tested on raw data without any initial data pre-selection in order to closely replicate real-time data streaming. When noise examples were included with the earthquake data, the CNN was found to be stable predicting accurately the ground shaking intensity corresponding to the noise amplitude.