神经网络辅助研究:地震 "知道 "会有多大吗?

Neri Berman, Oleg Zlydenko, Oren Gilon, Yossi Matias, Yohai Bar-Sinai
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引用次数: 0

摘要

地震的发生是出了名的难以预测。虽然点过程模型可以较好地捕捉到地震时空统计的某些方面,但对未来事件的震级却知之甚少,而且在地震发生之前预测其震级是否可能还存在很大争议。这既是由于缺乏有关断层条件的信息,也是由于破裂动力学本身的复杂性。因此,即使是最先进的预测模型,除了与时间无关的古腾堡-里克特(GR)分布(该分布描述了地震在大区域和长时间内的边际分布)之外,通常也不会对未来事件的震级有所了解。这种方法隐含地假定地震震级与之前的地震活动无关,并且是同分布的。在这项研究中,我们挑战了这一观点,证明可以直接从地震历史中提取即将发生地震的震级信息。我们提出了 MAGNET - MAGnitudeNeural EsTimation 模型,这是一个开源的、受地球物理启发的神经网络模型,用于从编目属性(即过去地震的震中位置、发生时间和震级)对未来震级进行概率预测。在南加州、日本和新西兰的实际地震目录中,我们的历史依赖模型优于基于 GR 的静态和准静态基准。这表明地震目录包含了未来地震发生前的震级信息。最后,我们提出了将该模型应用于地震准备阶段的特征描述以及实用危险警报和地震预报系统的方法。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Do earthquakes "know" how big they will be? a neural-net aided study
Earthquake occurrence is notoriously difficult to predict. While some aspects of their spatiotemporal statistics can be relatively well captured by point-process models, very little is known regarding the magnitude of future events, and it is deeply debated whether it is possible to predict the magnitude of an earthquake before it starts. This is due both to the lack of information about fault conditions and to the inherent complexity of rupture dynamics. Consequently, even state of the art forecasting models typically assume no knowledge about the magnitude of future events besides the time-independent Gutenberg Richter (GR) distribution, which describes the marginal distribution over large regions and long times. This approach implicitly assumes that earthquake magnitudes are independent of previous seismicity and are identically distributed. In this work we challenge this view by showing that information about the magnitude of an upcoming earthquake can be directly extracted from the seismic history. We present MAGNET - MAGnitude Neural EsTimation model, an open-source, geophysically-inspired neural-network model for probabilistic forecasting of future magnitudes from cataloged properties: hypocenter locations, occurrence times and magnitudes of past earthquakes. Our history-dependent model outperforms stationary and quasi-stationary state of the art GR-based benchmarks, in real catalogs in Southern California, Japan and New-Zealand. This demonstrates that earthquake catalogs contain information about the magnitude of future earthquakes, prior to their occurrence. We conclude by proposing methods to apply the model in characterization of the preparatory phase of earthquakes, and in operational hazard alert and earthquake forecasting systems.
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