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SISMIKO: emergency network deployment and data sharing for the 2016 central Italy seismic sequence

机译:SISMIKO:2016年意大利中部地震序列的应急网络部署和数据共享

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At 01:36 UTC (03:36 local time) on August 24th 2016, an earthquake Mw 6.0 struck an extensive sector of the central Apennines (coordinates: latitude 42.70° N, longitude 13.23° E, 8.0 km depth). The earthquake caused about 300 casualties and severe damage to the historical buildings and economic activity in an area located near the borders of the Umbria, Lazio, Abruzzo and Marche regions. The Istituto Nazionale di Geofisica e Vulcanologia (INGV) located in few minutes the hypocenter near Accumoli, a small town in the province of Rieti. In the hours after the quake, dozens of events were recorded by the National Seismic Network (Rete Sismica Nazionale, RSN) of the INGV, many of which had a ML 3.0. The density and coverage of the RSN in the epicentral area meant the epicenter and magnitude of the main event and subsequent shocks that followed it in the early hours of the seismic sequence were well constrained. However, in order to better constrain the localizations of the aftershock hypocenters, especially the depths, a denser seismic monitoring network was needed. Just after the mainshock, SISMIKO, the coordinating body of the emergency seismic network at INGV, was activated in order to install a temporary seismic network integrated with the existing permanent network in the epicentral area. From August the 24th to the 30th, SISMIKO deployed eighteen seismic stations, generally six components (equipped with both velocimeter and accelerometer), with thirteen of the seismic station transmitting in real-time to the INGV seismic monitoring room in Rome. The design and geometry of the temporary network was decided in consolation with other groups who were deploying seismic stations in the region, namely EMERSITO (a group studying site-effects), and the emergency Italian strong motion network (RAN) managed by the National Civil Protection Department (DPC). Further 25 BB temporary seismic stations were deployed by colleagues of the British Geological Survey (BGS) and the School of Geosciences, University of Edinburgh in collaboration with INGV. All data acquired from SISMIKO stations, are quickly available at the European Integrated Data Archive (EIDA). The data acquired by the SISMIKO stations were included in the preliminary analysis that was performed by the Bollettino Sismico Italiano (BSI), the Centro Nazionale Terremoti (CNT) staff working in Ancona, and the INGV-MI, described below.
机译:在2016年8月24日世界标准时间(UTC)01:36(当地时间03:36),亚平宁山脉中部发生了6.0级地震(坐标:北纬42.70°,东经13.23°,深度8.0 km)。地震在翁布里亚,拉齐奥,阿布鲁佐和马尔凯地区边界附近的地区造成约300人伤亡,并对历史建筑和经济活动造成严重破坏。国立地理大学(Vulcanologia)(Instituto Nazionale di Geofisica e Vulcanologia(INGV))在几分钟之内就位于埃蒂(Rieti)省一个小镇Accumoli附近的震中。地震发生几小时后,INGV的国家地震台网(Res Sismica Nazionale,RSN)记录了数十起事件,其中许多事件的ML> 3.0。 RSN在震中区域的密度和覆盖范围意味着主要事件的震中和震级以及在地震序列发生的最初几个小时中紧随其后的后续地震受到了很好的约束。但是,为了更好地限制余震震源的定位,特别是深度,需要一个更密集的地震监测网络。地震发生后不久,INGV应急地震网络的协调机构SISMIKO被激活,以便在震中地区安装与现有永久性网络集成的临时地震网络。从8月24日至30日,SISMIKO部署了18个地震台,通常由六个部件组成(配备了速度计和加速度计),其中13个地震台实时传输到罗马的INGV地震监测室。临时网络的设计和几何形状是与正在该地区部署地震台站的其他小组,即EMERSITO(研究场地影响的小组)和由意大利国家民航局管理的意大利紧急强运动网络(RAN)共同决定的。保护部门(DPC)。英国地质调查局(BGS)和爱丁堡大学地球科学学院的同事与INGV合作,又部署了25个BB临时地震台。从SISMIKO站获取的所有数据都可以在欧洲综合数据档案库(EIDA)中快速获得。 SISMIKO站获取的数据包括在Bollettino Sismico Italiano(BSI),在安科纳(Ancona)工作的Nazionale Terremoti中心(CNT)以及INGV-MI进行的初步分析中,如下所述。

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