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FUSION OF MULTI PRECURSORS EARTHQUAKE PARAMETERS TO ESTIMATE THE DATE, MAGNITUDE AND AFFECTED AREA OF THE FORTHCOMING POWERFUL EARTHQUAKES

机译:多前体融合的地震参数估算即将到来的强大地震的日期,幅度和影响地区

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Since not any individual precursor can be used as an accurate stand alone means for the earthquake prediction, it is necessary to integrate different kinds of precursors. The precursors selected for analysis in this study include electron and ion density, electron temperature, total electron content (TEC), electric and magnetic fields and land surface temperature (LST) several days before three strong earthquakes which happened in Samoa Islands, Sichuan (China) and Borujerd (Iran). The precursor's variations were monitored using data obtained from experiments onboard DEMETER (IAP, ISL, ICE and IMSC) and Aqua-MODIS satellites. Regarding the ionospheric precursors, the geomagnetic indices D_(st) and K_(p) were used to distinguish pre-earthquake disturbed states from the other anomalies related to the geomagnetic activities. The inter-quartile range of data was utilized to construct their upper and lower bound to detect disturbed states outsides the bounds which might be associated with impending earthquakes. When the disturbed state associated with impending earthquake is detected, based on the type of precursor, the number of days relative to earthquake day is estimated. Then regarding the deviation value of the precursor from the undisturbed state the magnitude of impending earthquake is estimated. The radius of the affected area is calculated using the estimated magnitude and Dobrovolsky formula. In order to assess final earthquake parameters (which are date, magnitude and radius of the affected area) for each case study, using the median and inter-quartile range of earthquake parameters obtained from different precursors, the approximate bounds of final earthquake parameters are defined. For each studied case, a good agreement was found between the estimated and registered earthquake parameters.
机译:由于不是任何单独的前体可以用作地震预测的精确站点,因此必须整合不同种类的前体。在本研究中选择用于分析的前体包括电子和离子密度,电子温度,总电子含量(TEC),电磁场,电场和磁场温度(LST)在四川萨摩亚群岛发生的三次强烈地震前几天(中国)(中国) )和Borujerd(伊朗)。使用从Demeter(IAP,ISL,ICES)和Aqua-Modis卫星的实验获得的数据进行监测前体的变化。关于电离层前体,地质磁性指数D_(ST)和K_(P)用于区分地震前的扰动状态与与地磁活动有关的其他异常。间隔的数据范围用于构建其上限和下限以检测受干扰状态,这些界限可能与即将到来的地震相关联。当检测到与即将发生地震相关的受干扰状态,基于前体的类型,估计相对于地震日的天数。然后,关于从未受干扰的状态的前体的偏差值估计即将发生的地震的大小。使用估计的幅度和Dobrovolsky公式计算受影响区域的半径。为了评估每种案例研究的最终地震参数(这是受影响区域的日期,幅度和半径),使用从不同前体获得的中位和四分位的地震参数范围,定义了最终地震参数的近似范围。对于每个研究的案例,估计和注册的地震参数之间发现了一个良好的一致性。

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