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The Assesement of Rip Current at Kerachut Beach Using Hydrodynamic Modelling

机译:利用流体动力学建模评估角裂海滩撕裂电流

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KerachutBeach is a beautiful beach in Penang National Park (PNP). However this beach is categorisedas one of dangerous beach for swimming activities in Malaysia due to the drowning incidents reported almost every year. The steep beach slope and rip current were among the factors that lead to this incident. Using bathymetry profile, current, tidal and sediment data collected at site incorporated with UKMO wave data analysis,the hydrodynamic pattern was simulated using Mike 21 modelling software. Result from the model showed the evidence of rip current existence along the coastline. It showed that this rip current eventsoccurred during spring tide phase when the flow change from Flood to Ebb. During this period, the current tend to move parallel to the shoreline with maximum speed of 0.3m/s which is capable to swipe away a swimmer. The bathymetry profile at Kerachutis very steep and dangerous to swimmers since there is a 4 meter sudden plunge just meters away from the shoreline.
机译:Kerachutbeach是槟城国家公园(PNP)的美丽海滩。 然而,由于溺水事件几乎每年报告,这个海滩是危险的游泳活动之一,即马来西亚的游泳活动。 陡峭的海滩坡和撕裂电流是导致这一事件的因素之一。 使用帕米波数据分析的站点收集的沐浴曲线型材,电流,潮汐和沉积物数据,使用Mike 21建模软件模拟了流体动力学模式。 该模型的结果显示了沿着海岸线撕裂电流存在的证据。 它表明,当流量从洪水变为潮流时,春天潮汐相位期间,该撕裂电流发生在春潮期间。 在此期间,电流倾向于平行于海岸线,最大速度为0.3米/秒,能够扫除游泳运动员。 Kerachutis的沐浴曲线概念非常陡峭,对游泳者危险,因为距离海岸线仅有4米的距离。

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