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首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >Application of real-time GPS to earthquake early warning in subduction and strike-slip environments
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Application of real-time GPS to earthquake early warning in subduction and strike-slip environments

机译:俯冲和走滑环境中实时GPS在地震预警中的应用

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摘要

We explore the application of GPS data to earthquake early warning and investigate whether the coseismic ground deformation can be used to provide fast and reliable magnitude estimations and ground shaking predictions. We use an algorithm to extract the permanent static offset from GPS displacement time series and invert for the slip distribution on the fault plane, which is discretized into a small number of rectangular patches. We developed a completely "self-adapting" strategy in which the initial fault plane model is built based on a quick, approximate magnitude estimation and is then allowed to increase in size based on the evolutionary magnitude estimation resulting from the slip inversion. Two main early warning outputs are delivered in real-time: magnitude and the along-strike extent of the rupture area. These are finally used to predict the expected ground shaking due to the finite source. We tested the proposed strategy by simulating real-time environments for three earthquakes. For the M_w 9.0, 2011 Tohoku-Oki earthquake, our algorithm provides the first magnitude estimate of 8.2 at 39 s after the origin time and then gradually increases to 8.9 at 120 s. The estimated rupture length remains constant from the outset at ~360 km. For the M_w 8.3, 2003 Tokachi-Oki earthquake, the initial magnitude estimate is 8.5 at 24 s and drops to 8.2 at 40 s with a rupture length of 290 km. Finally, for the M_w 7.2, 2010 El Mayor-Cucapah earthquake, the magnitude estimate is 7.0 from the outset with a rupture length of 140 km. The accuracy of the ground shaking prediction using the GPS-based magnitude and finite extent is significantly better than existing seismology-based point source approaches. This approach would also facilitate more rapid tsunami warnings.
机译:我们探索了GPS数据在地震预警中的应用,并研究了同震地面变形是否可用于提供快速,可靠的震级估算和地震动预测。我们使用一种算法从GPS位移时间序列中提取永久静态偏移量,并将其反演为断层平面上的滑动分布,并将其离散化为少量矩形块。我们开发了一种完全“自适应”的策略,在该策略中,基于快速的近似震级估算建立了初始断层平面模型,然后根据滑移反演产生的演化震级估算,允许其增大尺寸。实时提供两个主要的预警输出:破裂区域的大小和沿走向。最后将这些用于预测由于有限源而引起的预期地面震动。我们通过模拟三个地震的实时环境来测试所提出的策略。对于2011年东北冲绳9.0级地震,我们的算法在原始时间39 s时提供了8.2的首次震级估计,然后在120 s时逐渐增加到8.9震级估计。估计的破裂长度从一开始就保持恒定在〜360 km。对于2003年的十胜冲木8.3级地震,初始震级估计值为24秒8.5,而40秒则降至8.2 km,破裂长度为290 km。最后,对于2010年El Mayor-Cucapah的M_w 7.2级地震,一开始的震级估计为7.0,破裂长度为140 km。使用基于GPS的震级和有限程度进行地震动预测的准确性明显优于现有的基于地震学的点源方法。这种方法还将促进更迅速的海啸预警。

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