Survey of 2011 Tohoku earthquake tsunami inundation and run-up
Survey of 2011 Tohoku earthquake tsunami inundation and run-up
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DOI：
10.1029/2011gl049210
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发表时间：
2011-09-27
影响因子：
5.2
通讯作者：
Yanagisawa, Hideaki
中科院分区：
文献类型：
--
作者：
Mori, Nobuhito;Takahashi, Tomoyuki;Yanagisawa, Hideaki
2011年3月11日，当地时间14：46，日本东北海岸发生了9.0级地震。这次地震产生了一场海啸，袭击了日本以及太平洋周围的各个地点。随着来自日本各地的研究人员的参与，联合研究小组在日本海岸的2000公里上进行了一项海啸调查。迄今为止，已经对5300多个地点进行了调查，这是世界上最大的海啸调查数据集。在仙台平原上，最大淹没高度为19.5 m，海啸孔在内陆繁殖超过5 km。沿着仙台以北约50到200公里的RIA海岸，狭窄的海湾集中了海啸浪潮，产生了最大的淹没高度和奔跑。调查数据清楚地显示了海啸特征的区域依赖性。引用：莫里（N. res。 Lett。，38，L00G14，DOI：10.1029/2011GL049210。
At 14: 46 local time on March 11, 2011, a magnitude 9.0 earthquake occurred off the coast of northeast Japan. This earthquake generated a tsunami that struck Japan as well as various locations around the Pacific Ocean. With the participation of researchers from throughout Japan, joint research groups conducted a tsunami survey along a 2000 km stretch of the Japanese coast. More than 5300 locations have been surveyed to date, generating the largest tsunami survey dataset in the world. On the Sendai Plain, the maximum inundation height was 19.5 m, and the tsunami bore propagated more than 5 km inland. Along the ria coast from about 50 to 200 km north of Sendai, the narrow bays focused the tsunami waves, generating the largest inundation heights and run-ups. The survey data clearly show a regional dependence of tsunami characteristics. Citation: Mori, N., T. Takahashi, T. Yasuda, and H. Yanagisawa (2011), Survey of 2011 Tohoku earthquake tsunami inundation and run-up, Geophys. Res. Lett., 38, L00G14, doi:10.1029/2011GL049210.