Reference GNSS Stations for Warning on Possibility of Upcoming Earthquake in Zagreb

N. Solarić, M. Solarić, M. Marjanović, Zlatko Bogdanovski, Sasho Dimeski
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Abstract

Distances between permanent GNSSS stations in positional systems are usually short between 30 km and 80 km. So calculated distances between the GNSS stations from their position coordinates calculated by processing collected GNSS data with Bernese software will be very well determined. The first time we determined that two days before earthquake in Kraljevo 2010 were shortening of sides between the GNSS referent stations, that this was a compression of the Earth’s crust two days before the earthquake. This effect was also confirmed on the Earthquakes Dreznica 2013, Skopje 2016 and Zagreb 2018 and that after compression two or several days after the earthquake occurs. However, they can also enable geophysicists to determine warn of possible earthquakes. On the end it was suggested that in the Control Center of CROPOS is required to establish a department for determination of compression in Earth crust based on GNSS measurement of the reference GNSS stations. This compression is possible to determine by "The method of daily changing the distance between GNSS permanent referent stations". After determination compression in Earth crust and using other geophysical methods will be probably possible to warn to upcoming earthquakes.
参考GNSS站对萨格勒布即将发生地震的可能性进行预警
定位系统中永久GNSSS站之间的距离通常在30公里至80公里之间。因此,用伯尔尼软件处理收集的GNSS数据计算出的GNSS站之间的位置坐标计算出的距离将很好地确定。我们第一次确定2010年克拉列沃地震前两天GNSS参考站之间的边缩短,这是地震前两天地壳的压缩。在2013年德雷兹尼察地震、2016年斯科普里地震和2018年萨格勒布地震中,以及地震发生后两天或几天的压缩后,也证实了这种效应。然而,它们也可以使地球物理学家确定可能发生地震的预警。最后,建议在CROPOS控制中心建立一个以参考GNSS站的GNSS测量为基础的地壳压缩测定部门。这种压缩可以通过“每日改变GNSS永久参考站之间距离的方法”来确定。在确定地壳的压缩和使用其他地球物理方法后,可能会对即将到来的地震发出警告。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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