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Statistical Comparison of National Probabilistic Seismic Hazard Maps and Frequency of Recorded JMA Seismic Intensities from the K-NET Strong-motion Observation Network in Japan during 1997–2006

机译:1997-2006年日本K-NET强震观测网络全国概率地震灾害图和记录的JMA地震烈度频率的统计比较

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National seismic hazard maps for Japan with meshes of 1x1 km2 were published by the Earthquake Research Committee of Japan in March 2005. They are updated annually to reflect time passage of event recurrence (NIED 2005). Since the probabilistic seismic hazard maps focus on estimates for 30 and even 50 years, strict validation of the maps requires probabilistic and statistical approaches with future data. Nevertheless, in this study, as the first step in verifying the validity of the maps, we compared the Japan Meteorological Agency (JMA) instrumental intensities from strong-motion records for the 10-year period ending 31 December 2006 with the corresponding values on the probabilistic hazard maps. The JMA instrumental intensity is a cumulative strong motion indicator, which was adjusted to match the scale previously used to measure seismic intensity, which was based on human response and an index of damage. The JMA intensity scale has 10 grades from 0 to 7 (5 and 6 were divided in lower and higher) and is described at http://www.jma.go.jp/jma/kishou/know/shindo/shindokai.html. Explanations of individual intensities can be found at http://www.jma.go.jp/jma/kishou/know/shindo/explane.html. Although corresponding peak ground acceleration could not precisely be adapted to the intensity scale, relative peak ground acceleration is indicated in http://en.wikipedia.org/wiki/Japan_Meteorological_Agency_seismic_intensity_scale. JMA has promptly reported this intensity since April 1996 (http://www.jma.go.jp/en/quake/).
机译:日本地震研究委员会于2005年3月发布了网格为1x1 km2的日本国家地震灾害图。该图每年更新一次,以反映事件复发的时间流逝(NIED 2005)。由于概率地震灾害图的重点是30年甚至50年的估计,因此严格验证这些图需要使用未来数据的概率和统计方法。不过,在本研究中,作为验证地图有效性的第一步,我们将日本气象厅(JMA)的强强度记录中截至2006年12月31日的10年期间的仪器强度与相应的值进行了比较。概率危害图。 JMA仪器强度是一个累积的强烈运动指示符,已根据人的反应和破坏指数进行了调整,以匹配以前用于测量地震强度的标度。 JMA强度等级从0到7有10个等级(5和6分为较低和较高的等级),并在http://www.jma.go.jp/jma/kishou/know/shindo/shindokai.html中进行了描述。可以在http://www.jma.go.jp/jma/kishou/know/shindo/explane.html上找到有关单个强度的说明。尽管无法将相应的峰值地面加速度精确地调整为强度标尺,但相对峰值地面加速度在http://en.wikipedia.org/wiki/Japan_Meteorologic_Agency_seismic_intensity_scale中指示。自1996年4月以来,JMA迅速报告了这种强度(http://www.jma.go.jp/en/quake/)。

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