Calibration of shaking intensity models of the “Extremum” system to simulate loss due to the 2020 Croatia earthquakes

IF 0.9 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Geofizika Pub Date : 2022-01-24 DOI:10.15233/gfz.2021.38.8
S. Markušić, N. Malaeva, S. Suchshev, I. Gabsatarova, N. Frolova
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Abstract

This paper is devoted to applications of the “Extremum” loss simulation system to two damaging earthquakes which occurred in Croatia in 2020. We provide a calibration procedure of mathematical models used for shaking intensity simulation. The regional macroseismic field parameters, such as the coefficients in the macroseismic field equation; the ratio between the longer (b) and the shorter (a) axes of the higher elliptical isoseismals (the flattening ratio k); the angle that specifies the orientation of the macroseismic field, in particular, the azimuth of the longer axis in the isoseismal ellipse, were all based on extensive macroseismic data acquired for the Balkan region and on the data for an analogous area with similar seismotectonic parameters in the Caucasus. We obtained a fairly good consistency between the results of simulation applied to the impact of the 2020 Croatia earthquakes and observations, confirming that the calibration of the macroseismic model by the Extremum system was both reasonable and effective for enhancing reliability for real time loss estimation.
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校准“极值”系统的震动强度模型,以模拟2020年克罗地亚地震造成的损失
本文研究了“极值”损失模拟系统在2020年克罗地亚两次破坏性地震中的应用。我们提供了一个用于振动强度模拟的数学模型的校准程序。区域大地震场参数,如大地震场方程中的系数;高椭圆等震线的长轴(b)与短轴(a)之比(平坦比k);指定大地震场方向的角度,特别是等震椭圆中较长轴的方位角,都是基于在巴尔干地区获得的大量大地震数据以及在高加索地区具有类似地震构造参数的类似地区的数据。应用于2020年克罗地亚地震影响的模拟结果与观测结果具有较好的一致性,证实了Extremum系统对大地震模型的校准是合理有效的,可以提高实时损失估计的可靠性。
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来源期刊
Geofizika
Geofizika 地学-地球化学与地球物理
CiteScore
1.60
自引率
0.00%
发文量
17
审稿时长
>12 weeks
期刊介绍: The Geofizika journal succeeds the Papers series (Radovi), which has been published since 1923 at the Geophysical Institute in Zagreb (current the Department of Geophysics, Faculty of Science, University of Zagreb). Geofizika publishes contributions dealing with physics of the atmosphere, the sea and the Earth''s interior.
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