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Real-Time Assessment of the 16 September 2015 Chile Tsunami and Implications for Near-Field Forecast

机译:2015年9月16日智利海啸实时评估及其对近场预报的影响

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The magnitude 8.3 earthquake in central Chile on 16 September 2015 and the resulting tsunami severely affected the region, with 15 deaths (Onemi in Monitoreo por sismo de mayor intensidad. (In Spanish) , 2015), over one million evacuated, and flooding in nearby coastal cities. We present our real-time assessment of the 2015 Chile tsunami using the Short-term Inundation Forecasting for Tsunamis system, and post-event analyses with local community models in Chile. We evaluate three real-time tsunami sources, which were inverted at the time that the first quarter-, half-, and full-wave passed the first tsunameter (DART 32402, located approximately 580 km north-northwest of the epicenter), respectively. Measurement comparisons from 26 deep-ocean tsunameters and 38 coastal tide stations show that good model accuracies are achieved for all three sources, particularly for the local sites that recorded the most destructive waves. The study highlights the forecast speed, time and accuracy dependence, and their implications for the local forecast capability. Our analyses suggest that the tsunami's main origination area is about 100-200 km long and 100 km wide, to the north of the earthquake epicenter along the trench and the total estimated tsunami wave energy is 7.9 x 10(13) J (with 13 % uncertainty). The study provides important guidelines for the earliest reliable estimate of tsunami energy and local forecasts. They can be obtained with the first quarter-wave of tsunameter recording. These results are also confirmed by a forecast analysis of the 2011 Japan tsunami. Furthermore, we find that the first half-wave tsunameter data are sufficient to accurately forecast the 2015 Chile tsunami, due to the specific orientation between the nearest tsunameter and the source. The study also suggests expanding the operational use of the local community models in real time, and demonstrates the applicability of the model results for "all-clear" evaluations, search and rescue operations, and near-real-time mitigation planning in both near and far fields.
机译:2015年9月16日在智利中部发生的8.3级地震和随之而来的海啸严重影响了该地区,造成15人死亡(Onemi in Monitoreo por sismo de Mayor intensidad。(西班牙语),2015年),超过100万人撤离,附近洪水泛滥沿海城市。我们使用海啸系统的短期淹没预测,以及智利当地社区模型的事后分析,对2015年智利海啸进行了实时评估。我们评估了三个实时海啸源,分别在第一个四分之一,一半和全波通过第一个tsunameter(DART 32402,位于震中西北西北约580公里)时反转。来自26个深海tsunameters和38个沿海潮汐台站的测量比较表明,所有三个源都获得了良好的模型精度,特别是对于那些破坏性最强的海浪站点。该研究突出了预测速度,时间和准确性的依赖性,以及它们对本地预测能力的影响。我们的分析表明,海啸的主要震源区长约100-200 km,宽100 km,位于地震震中中心沿海沟的北部,总海啸波能量估计为7.9 x 10(13)J(占13%不确定)。该研究为海啸能源的早期可靠估计和当地预报提供了重要指导。它们可以在tsunameter录音的第一个四分之一波中获得。 2011年日本海啸的预测分析也证实了这些结果。此外,我们发现,由于最近的tsunameter和震源之间的特定方向,前半波tsunameter数据足以准确预测2015年智利海啸。该研究还建议实时扩展本地社区模型的操作用途,并展示该模型结果在“近距离”和“近距离”减灾规划中的“全清晰”评估,适用性和适用性。遥远的领域。

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