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Video Content Analysis of the 2018 Sulawesi Tsunami, Indonesia: Impact at Palu Bay

机译:2018年Sulawesi海啸,印度尼西亚的视频内容分析:在Palu Bay的影响

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Water surface disturbances at two locations were captured by two separate witness videos few minutes before the Sulawesi tsunami hit the Palu City, Indonesia on Sep 28, 2018. One of these videos shows top-view of both locations with surface disturbances. The other video shows the side-view of one of the locations with surface disturbance (also recorded in the top-view video), as a fast-moving bore (broken wave with splash). This work performs a Video Content Analysis (VCA) to locate these surface disturbances and to give a rough estimate of the wave characteristic and evolution when the videos were recorded. For the top-view video, VCA was done on a single frame that depicts two observable areas of tsunami generation with a pair of tall sharp-crested waves (unbroken waves). Width of the wave fronts and height of the tall sharp-crested waves are determined using this selected frame. For the side-view video, a sequence of video frames were used to determine the splash height, wave speed and acceleration of the fast-moving bore. In addition, our work points out some similar wave characteristics between the tall sharp-crested waves observed in the videos and waves generated by a submarine landslide lab experiment from the literature. Using simple tools, e.g., Google Earth for three-dimension measurement and satellite view and basic geometrical optics methods, we give a rough estimate of the wave size, velocity and acceleration during the recorded time. As per the results, the observable tall sharp-crested wave fronts have approximate widths of 383 and 461 m and crest-trough heights about 24 and 29 m. The fast-moving bore has an average speed of approximately 22 m/s (78 km/h) with an acceleration of similar to 1:18 m/s(2). This work provides information which cannot be retrieved by post-event field survey, and we consider that the information could be useful for numerical modelers to validate their simulations, sources and model physics by comparing quantitatively to res
机译:在2018年9月28日之前,在Sulawesi海啸前几分钟捕获了两个单独的见证视频的水面扰动。其中一个视频之一显示了两种地点干扰的顶部视图。另一个视频显示了具有表面干扰的一个位置的侧视图(也记录在顶视图中),作为快速移动的孔(带飞溅的破碎波)。该工作执行视频内容分析(VCA)以定位这些表面干扰,并在记录视频时对波特性和演变进行粗略估计。对于顶视图视频,VCA是在一个帧上完成的,描绘了海啸的两个可观察区域,具有一对高大的尖锐波浪(不间断的波浪)。使用该所选框架确定高尖锐波浪的波前沿的宽度和高度的尖锐波浪的高度。对于侧视视频,使用一系列视频帧来确定快速移动孔的飞溅高度,波速度和加速度。此外,我们的工作指出了在由文献中由潜艇滑坡实验室实验生成的视频和波浪中观察到的高大尖锐波浪之间的一些类似的波浪特征。使用简单工具,例如Google地球用于三维测量和卫星视图和基本的几何光学方法,我们在录制的时间内粗略估计波浪尺寸,速度和加速度。根据结果​​,可观察到的高大尖锐波浪前沿的宽度为383和461米,冠长高度约24和29μm。快速移动的孔的平均速度约为22米/秒(78km / h),加速度与1:18 m / s(2)相似。这项工作提供了由事件后现场调查无法检索的信息,我们认为该信息对于数值设计师来说是有用的,以通过定量与RES进行比较来验证其模拟,来源和模型物理学

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