首页> 外文会议>International Symposium on Coastal Engineering and Science of Coastal Sediment Processes >BEACH MORPHOLOGY AT BANDA ACEH, INDONESIA IN RESPONSE TO THE TSUNAMI ON 26 DECEMBER 2004
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BEACH MORPHOLOGY AT BANDA ACEH, INDONESIA IN RESPONSE TO THE TSUNAMI ON 26 DECEMBER 2004

机译:在2004年12月26日,印度尼西亚Banda Aceh的海滩形态,在2004年12月26日回应海啸

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A study of morphological response and development of beaches which were affected by the earthquake and the tsunami on 26th December 2004 has been conducted at two selected coastal sections of Banda Aceh, Indonesia, A simplified principle adopted from one-line shoreline theory in a geospatial analysis utilizing identified shoreline features across the foreshore zone is applied,. The analysis yields a rough estimation of the shoreline and sediment volume changes since the tsunami After the severe impact as revealed by a significant chaotic shoreline retreat, the morphological development in the following 6 months has shown that about 15% of the total sediment loss due to the tsunami on the northwest coast has further been eroded, while 60% of that on the west coast has been compensated by accretion. This leads to a conclusion that different coastal characteristics show different responses to, and developments after the tsunami.
机译:在2004年12月26日,印度尼西亚班达·亚齐的两个选定的沿海部分进行了一项受地震和海啸的形态反应和发展的研究,这是一种在地理空间分析中采用一线海岸线理论采用的简化原则利用跨越公共区域的所识别的海岸线特征。分析产生自海啸后海岸线和沉积物体积变化的粗略估计,因为在严重的混乱海岸线撤退后的严重影响之后,后续6个月的形态学发育表明,由于沉积物损失的约15%西北海岸的海啸进一步被侵蚀,而西海岸的60%已被吸收赔偿。这导致得出的结论是,不同的沿海特征显示海啸后的不同反应和发展。

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