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首页> 外文期刊>Remote Sensing of Environment: An Interdisciplinary Journal >Assessing the potential of thermal infrared satellite surveys for monitoring seismically active areas: The case of Kocaell (Izmit) earthquake, August 17, 1999
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Assessing the potential of thermal infrared satellite surveys for monitoring seismically active areas: The case of Kocaell (Izmit) earthquake, August 17, 1999

机译:评估红外热卫星勘测潜在地震活动区域的潜力:1999年8月17日Kocaell(伊兹密特)地震案例

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摘要

Space-time anomalies of Earth's emitted radiation in the thermal infrared spectral range (TIR) measured from satellite months to weeks before the occurrence of earthquakes, have been interpreted, by several authors, as pre-seismic signals. The claimed connection of TIR emission with seismic activity has been considered, up to now, with some caution by the scientific community mainly for the insufficiency of the validation data-sets and the scarce importance attached by those authors to other causes (e.g. meteorological) that, rather than seismic activity, could be responsible for the observed TIR signal fluctuations.In this paper, a robust satellite data analysis technique is described which pen-nits us to identify anomalous space-time TIR signal transients even in very variable observational (satellite view angle, land topography and coverage, etc.) and natural (e.g. meteorological) conditions. A statistically well-founded definition of TIR anomaly is given and proposed as a suitable tool for satellite TIR surveys in seismically active regions. Eight years of Meteosat TIR observations have been analyzed in order to characterize the TIR signal behavior at each specific observation time and location. Space-time TIR signal transients have then been analyzed, both in the presence (validation) and in the absence of (confutation) seismic events, looking for possible space-time relationships. The devastating earthquake which occurred in Turkey (Izmit.. August 17, M(S)similar to 7.8) in 1999 has been considered as a test case for validation, relatively unperturbed periods (no earthquakes with M > 5) were taken for confutation purposes. Quite intense (S/N > 3.5) and rare, spatially extensive and time persistent, TIR signal transients were identified appearing eight days before the Izmit main shock in Greece, moving to Turkey on August 13 and disappearing, moving back to Greece, some days after. Possible implications of such results, together with present limitations of the proposed technique, will also be discussed in the light of the improved performances expected by its extension to other existing or future satellite packages. (c) 2005 Elsevier Inc. All rights reserved.
机译:几位作者已经将地震发生前几个月到几周内在红外光谱范围内测量的地球辐射辐射的时空异常,解释为地震前信号。直到现在,TIR辐射与地震活动之间的联系都得到了考虑,科学界一直在谨慎考虑,主要是因为验证数据集不足以及这些作者对其他原因(例如气象学)的重视不足而不是地震活动可能是造成观测到的TIR信号波动的原因。本文描述了一种可靠的卫星数据分析技术,即使在观测条件非常变化的情况下(卫星视图),我们也能识别出异常的时空TIR信号瞬变角度,陆地地形和覆盖范围等)和自然(例如气象)条件。给出了TIR异常的统计学依据,并被定义为地震活跃地区卫星TIR勘测的合适工具。已分析了八年的Meteosat TIR观测结果,以表征每个特定观测时间和位置的TIR信号行为。然后,在存在(验证)和不存在(配置)地震事件的情况下,对时空TIR信号瞬态进行了分析,以寻找可能的时空关系。 1999年在土耳其发生的毁灭性地震(伊兹密特。8月17日,M(S)与7.8相似)被视为验证的测试用例,相对平稳的时期(没有M> 5的地震)被用于对冲目的。 TIR信号瞬变非常强烈(信噪比> 3.5),并且罕见,空间分布广泛且时间持续,在希腊的伊兹密特主震发生前八天出现了瞬态信号,8月13日移至土耳其,然后消失,几天后移回希腊后。这些结果的可能含义以及所提出技术的当前局限性,还将根据其扩展到其他现有或将来的卫星封装所期望的改进性能来进行讨论。 (c)2005 Elsevier Inc.保留所有权利。

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