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Ground tilt changes in Japan caused by the 2010 Maule, Chile, earthquake tsunami

机译:2010年智利莫尔地震海啸引起的日本地面倾斜变化

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Oscillating ground tilt perturbations accompanied by the 2010 Maule, Chile, earthquake tsunami were observed over a broad inland area facing the Pacific Ocean coast in Japan by a high-density tiltmeter network. Through an analysis of ground tilt data observed at more than 500 stations, we were able to obtain a detailed spatiotemporal distribution of the tsunami-induced tilt changes and reveal a relationship between the tilt amplitude and the distance from the coast. At distances of 1 km or less, the peak tilt amplitudes were ~5 × 10~(-2) μrad and were almost constant with respect to the distance. At distances greater than 3 km, amplitudes were inversely proportional to the distance and reached ~5 × 10~(-3) μrad approximately 50 km away from the coast. The dominant ground tilting directions were almost the same as the direction orthogonal to the coastline. These observed ground tilt changes and their characteristics were successfully modeled with a loading deformation caused by sea level variations accompanied by the tsunami. Applying a two-dimensional boxcar tsunami model to the observed data, we estimated the water volume per unit length of coast for the Maule earthquake tsunami to be 2-7 × 10~3 m~3/m within the distance of 14-20 km seaward of the coastline. Key points A dense wide-area tiltmeter network observed tsunami-induced inland tilting Observed tilt amplitude systematically depends on the distance from the coast Inland tilt data enables us to estimate spatial parameters of nearshore tsunami
机译:通过高密度倾斜仪网络,在面向日本太平洋海岸的广阔内陆地区,观察到伴随着2010年智利莫勒(Maule)地震海啸的振荡地面倾斜扰动。通过分析在500多个站点观测到的地面倾斜数据,我们能够获得海啸引起的倾斜变化的详细时空分布,并揭示倾斜幅度与距海岸的距离之间的关系。在1 km或更小的距离处,峰值倾斜幅度为〜5×10〜(-2)μrad,并且相对于该距离几乎恒定。在距离大于3 km时,振幅与该距离成反比,并且在距海岸约50 km处达到〜5×10〜(-3)μrad。主要的地面倾斜方向与与海岸线正交的方向几乎相同。这些观测到的地面倾斜变化及其特征已成功建模,其中海平面变化和海啸造成了荷载变形。将二维棚车海啸模型应用于观测数据,我们估计在14-20 km范围内,莫尔地震海啸的海岸每单位长度的水量为2-7×10〜3 m〜3 / m海岸线向海。要点密集的广域测斜仪网络观测到的海啸引起的内陆倾斜观测到的倾斜幅度系统地取决于距海岸的距离内陆倾斜数据使我们能够估算近海海啸的空间参数

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