Tasikmalaya地区Cipatujah海啸升势模拟及易损区分析

Tamara Centong Mandey, A. Ismanto, D. Sugianto, P. Purwanto, R. Widiaratih, G. Harsono
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引用次数: 0

摘要

西帕都雅是印度尼西亚西爪哇省塔西马来亚县的一个街道,是爪哇省南部地区因构造活动而受到重大破坏的地区之一,即2006年在努沙坎班甘和pangandaran之后发生的7.7级地震和西爪哇省海啸。根据2006年7月17日爪哇地震情景在西峇都雅的易损区。本研究采用的方法是定量的,需要测深数据、高点、2006年7月17日地震参数、潮汐数据、RBI地图和土地利用数据。海啸建模与数值模拟使用COMCOT v 1.7和MATLAB软件,以及Arc Map绘制海啸覆盖范围和易损区区域。经数据处理,最大波速为3.92 m/s。在第27分钟,海浪到达了西帕图亚地区,最大上升高度为6.115米,最大海啸范围为1.891米。根据对西帕图亚海啸覆盖数据的处理,受海啸影响的面积为11.64平方公里。而对于西帕图贾的海啸易损区,则分为低危险区、中危险区和高危险区3类。这表明西帕图亚地区属于海啸高易发区。基于RSR值为0.073的验证和验证结果,则假设在事件期间发生的助跑数据足以满足助跑模型的高度。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The Modeling of Tsunami Wave Run-Up and Vulnerability Zone Analysis In Cipatujah, Tasikmalaya District
Cipatujah is a sub-district in Tasikmalaya Regency, West Java Province, Indonesia, which is one of the areas affected by significant damage due to tectonic activity in the southern region of Java, namely an earthquake with a magnitude of 7.7 magnitude and West Java tsunami in 2006 after Nusa Kambangan and PangandaranThe purpose of this study is to estimate the tsunami travel time, wave heights distribution, coverage areas, and vulnerability zone based on the Java 17 July 2006 earthquake scenario in Cipatujah, Tasikmalaya Regency. The method used in this study is quantitative and requires bathymetry data, high points, earthquake parameters of July 17, 2006, tidal data, RBI maps, and land use data. Tsunami modeling with numerical simulations using COMCOT v 1.7 and MATLAB software, also Arc Map for mapping tsunami coverage and vulnerability zone areas. Based on data processing, it was found that the maximum wave speed of 3.92 m/s. In the 27th minute, the waves had reached the Cipatujah region, with a maximum run-up height of 6.115 meters and a maximum tsunami range on the land of 1.891 meters. The area affected by the tsunami based on the processing of tsunami coverage data in Cipatujah totals 11.64 km2. Whereas for tsunami vulnerability zone in Cipatujah, it is divided into 3 categories, namely low hazard zone, medium hazard zone, and high hazard zone. This indicates that the Cipatujah region is included in a high tsunami-prone zone. Based on the results of verification and validation with an RSR value of 0,073, then it is assumed that the height of the run-up model is sufficient by the run-up data that occurred during the event.  
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