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Earthquake signature revealed by time series satellite and ground-based data

机译:时间序列卫星和地面数据揭示了地震信号

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This paper presents observations based on in-situ and time series MODIS Terra/Aqua and NOAA-AVHRR satellite data on derived anomalies of multi geophysical parameters (land surface temperature -LST, outgoing long-wave radiation-OLR, and mean air temperature- AT for some seismic events recorded in Vrancea seismic region in Romania. Starting with almost one week prior to a moderate or strong earthquake a transient thermal infrared rise in LST of several Celsius degrees (℃) and the increased OLR values higher than the normal have been recorded around epicentral areas, function of the magnitude and focal depth, which disappeared after the main shock. A developed Lithosphere-Surfacesphere-Atmosphere-Ionosphere Coupling (LSAIC) model can explain most of these presignals as a synergy between different anomalies of geophysical/geochemical parameters. These anomalies prior to medium to strong earthquakes are attributed to the thermodynamic, degassing and ionization processes in the Earth- Atmosphere system and micro-fracturing in the rocks especially along area's active faults. The main outcome of this paper is an unified concept for systematic validation of different types of earthquake precursors of which Land Surface Temperature (LST), outgoing Long wave Radiation (OLR), Air Temperature (AT), radon gas concentration, are the most reliable parameters within the chain of the processes described by a LSAIC model.
机译:本文介绍了基于原位和时间序列MODIS Terra / Aqua和NOAA-AVHRR卫星数据的观测结果,这些数据涉及多个地球物理参数(陆地表面温度-LST,外向长波辐射-OLR和平均气温-AT)的导出异常记录了罗马尼亚Vrancea地震区发生的一些地震事件,从中度或强烈地震前将近一个星期开始,LST的瞬时热红外上升了几摄氏度(℃),并且OLR值比正常值要高。震中区域周围的震级和震源深度的函数在主震后消失,发达的岩石圈-地表球-大气-电离层耦合(LSAIC)模型可以解释大多数这些前兆信号是地球物理/地球化学参数不同异常之间的协同作用。中到强烈地震之前的这些异常现象是由于地球大气中的热力学,脱气和电离过程引起的这里是岩石中的系统和微裂缝,特别是沿该地区活动断层的裂缝。本文的主要成果是一个统一的概念,用于系统验证不同类型的地震前兆,其中最可靠的是地表温度(LST),外出长波辐射(OLR),气温(AT),ra气浓度LSAIC模型描述的过程链中的参数。

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