Robust Satellite Techniques for mapping thermal anomalies possibly related to seismic activity of March 2021, Thessaly Earthquakes.

M. Kouli, Sofia Peleli, V. Saltas, J. Makris, F. Vallianatos
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引用次数: 4

Abstract

In recent years, there is a growing interest concerning the development of a multi-parametric system for earthquakes’ short term forecast identifying those parameters whose anomalous variations can be associated to the complex process of such events. In this context, the Robust Satellite Technique (RST) has been adopted herein with the aim to detect and map thermal anomalies probably related with the strong earthquake of M6.3 occurred near the city of Larissa, Thessaly on March 3rd 2021 10:16:07 UTC. For this purpose, 10 years (2012-2021) of daily Night-time Land Surface Temperature (LST) remotely sensed data from Moderate Resolution Imaging Spectroradiometer (MODIS), were analyzed. Pixels characterized by statistically significant LST variations on a daily scale were interpreted as an indicator of variations in seismic activity. Quite intense (Signal/Noise ratio > 2.5) and rare, spatially extensive and time persistent, TIR signal transients were identified, appearing twenty five days before the Thessaly main shock (pre-seismic anomalies: February 6th, February 11th March 1st), the day of the main earthquake (co-seismic anomaly) and after the main shock (post-seismic anomalies: March 4th, 10th and 17th). The final dataset of thermal anomalies was combined with geological and structural data of the area of interest, such as active faults, composite seismogenic sources, earthquake epicenter and topography in order to perform preliminary spatial analysis.
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绘制可能与2021年3月地震活动相关的热异常的强大卫星技术,色萨利地震。
近年来,人们对开发地震短期预报的多参数系统越来越感兴趣,该系统可以识别那些异常变化可能与地震复杂过程有关的参数。在此背景下,本文采用稳健卫星技术(Robust Satellite Technique, RST),目的是探测和绘制可能与2021年3月3日10:16:07 UTC发生在色萨利拉里萨市附近的6.3级强烈地震相关的热异常。利用中分辨率成像光谱辐射计(MODIS) 10年(2012-2021)夜间地表温度(LST)遥感数据进行分析。在日尺度上以统计上显著的地表温度变化为特征的像元被解释为地震活动变化的指标。TIR信号强度大(信噪比> 2.5),且罕见、空间广泛、时间持久,分别出现在色sally主震前25天(震前异常:2月6日、2月11日、3月1日)、主震当日(同震异常)和主震后25天(震后异常:3月4日、10日和17日)。最终的热异常数据集将与研究区域的地质和构造数据(如活动断层、复合发震源、震中和地形)相结合,进行初步空间分析。
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