关于2018年9月28日印度尼西亚海啸及其原因的综合报告

Nazeel Sabah, Arjun Sil
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引用次数: 0

摘要

海啸是人类经历过的最致命的自然灾害之一。几个世纪以来,众所周知,海啸造成了巨大的破坏,造成了广泛的财产和生命损失。本报告涉及2018年9月28日的海啸,该海啸袭击了岛国印度尼西亚,特别是中苏拉威西岛。印度尼西亚位于太平洋火山带的地理位置使该国特别容易受到强烈海啸的影响。本研究中考虑的海啸是由7.5级(Mw)强烈地震引发的。通常情况下,走滑地震不会引发海啸,但这次海啸非常出乎意料,因为断层机制是走滑(沿帕卢-科罗断层走滑)。当地的地质、地理和构造构造是确定一个地区海啸危险性的关键参数。本报告试图探讨海啸发生的原因和机制。次级因素如漏斗效应和海湾效应、海底滑坡、液化和滑坡也会放大海啸的影响。该研究提供了与该事件相关的前震和余震的结论性说明。还试图通过比较卫星图像的时间线来研究所造成的损失、伤亡和其他损失。从1500年至今从各种目录中获得的数据集进行了统计研究,突出了突出的结果。
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A comprehensive report on the 28th September 2018 Indonesian Tsunami along with its causes

Tsunami is one of the deadliest natural disasters that mankind has ever experienced. Over the centuries, tsunami is known to have caused massive destruction owing to widespread loss and damage to property and human life. This report deals with the tsunami of 28th September 2018, which hit the Island nation of Indonesia, especially the Central Sulawesi Island. Indonesia's geographical location along the pacific ring of fire makes the nation exceptionally prone to strong tsunami. The tsunami under consideration in this study was triggered by a strong earthquake of magnitude (Mw) 7.5 scale. Usually, a strike-slip earthquake never leads to tsunami, but this tsunami was quite unexpected as the fault mechanism involved was strike-slip (strike slip along the Palu-Koro fault). The local geology, geography and tectonic configuration are crucial parameters in determining the tsunami hazard in an area. This report tries to examine the causative factors and mechanism behind the occurrence of tsunami. Secondary factors like funnelling and bay effect, submarine landslips, liquefaction and landslides which could have amplified the effects of the tsunami are also presented. The study provides a conclusive account of the related foreshocks and aftershocks associated to the event. A study of the losses incurred, causalities and other losses has also been attempted by comparing a timeline of satellite imageries. A statistical study was made from the datasets obtained from various catalogues from 1500 till date and the salient results are highlighted.

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