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NEAR REAL-TIME DETERMINATION OF EARTHQUAKE SOURCE PARAMETERS FOR TSUNAMI EARLY WARNING FROM GEODETIC OBSERVATIONS

机译:海啸观测近期实时确定海啸预警的地震源参数

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Exemplifying the tsunami source immediately after an earthquake is the most critical component of tsunami early warning, as not every earthquake generates a tsunami. After a major under sea earthquake, it is very important to determine whether or not it has actually triggered the deadly wave. The near real-time observations from near field networks such as strong motion and Global Positioning System (GPS) allows rapid determination of fault geometry. Here we present a complete processing chain of Indian Tsunami Early Warning System (ITEWS), starting from acquisition of geodetic raw data, processing, inversion and simulating the situation as it would be at warning center during any major earthquake. We determine the earthquake moment magnitude and generate the centroid moment tensor solution using a novel approach which are the key elements for tsunami early warning. Though the well established seismic monitoring network, numerical modeling and dissemination system are currently capable to provide tsunami warnings to most of the countries in and around the Indian Ocean, the study highlights the critical role of geodetic observations in determination of tsunami source for high-quality forecasting.
机译:在地震发生后,海啸是海啸预警最关键的成分,而不是每种地震都会产生海啸。在海洋地震发生重大后,确定是否触发致命波浪是非常重要的。来自近场网络的近实时观察,如强大的运动和全球定位系统(GPS)允许快速确定故障几何形状。在这里,我们介绍了印度海啸预警系统(Itews)的完整加工链,从收购大地原始数据,加工,反转和模拟情况时,在任何重大地震期间都在警告中心。我们确定地震矩幅度,并使用一种新的方法产生质心矩张解液,这是海啸预警的关键要素。虽然良好的地震监测网络,数值建模和传播系统目前有能力向印度洋和周围的大多数国家提供海啸警告,但该研究突出了大地测量观测在高质量的测定中的影响预测。

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