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An early warning system for inundation forecast due to a tropical cyclone along the east coast of India

机译:印度东海岸的热带气旋导致的淹没预测预警系统

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摘要

Cyclone-induced coastal inundation along the east coast of India is simulated using the state-of-the-art advanced circulation model coupled with Simulating Waves Nearshore model. Bathymetry of the computational domain is prepared by integrating digital coastal bathymetric chart with global digital elevation model (DEM) ETOPO-2. Topography of the coastal land region is created by merging data from the fine resolution airborne DEM with that from the Indian satellite CARTOSAT-2 derived CARTO2 DEM and Shuttle Radar Topography Mission DEM. The major shortcomings of coastal inundation simulation due to inaccurate representation of intricate networks of river, creeks and lagoons have been overcome by careful description of the critical coastal wetland features influencing the landward inundation of storm surge in the present work. Experimental simulation of coastal inundation is carried out for the Phailin (2013) and Hudhud (2014) cyclones. The computed surge residual for Phailin and Hudhud are compared with available tide-gauge observations, which have resulted in root mean square error of 0.06 m and 0.11 m, respectively. The simulations show realistic coastal inundations, which are compared with the Indian meteorological department records. The model set up is then used to generate forecast of coastal inundation due to Titli (2018) cyclone with a lead period of 48 h. The Weather Research and Forecasting model forecast winds at 5 km spatial resolution are used as the primary forcing parameter. The coastal inundation forecast due to Titli cyclone is validated by assessing the spatial coherency of simulated inundation with the water logged area demarcated from synthetic-aperture radar image taken from Canadian satellite RADARSAT-2. The results clearly indicate acceptability of the model performance with a potential to predict the coastal inundation during a cyclone for operational early warning.
机译:使用与模拟波段近岸模型的模拟波耦合,模拟印度东海岸的旋风引起的沿海淹没。通过将数字沿海气候图表与全球数字高度模型(DEM)ETOPO-2集成来制备计算结构域的浴约定。沿海地区地区的地形是通过从印度卫星Cartosat-2衍生的Carto2 Dem和班车雷达形貌Mission DEM中的良好分辨率的空中灭虫DEM的数据来创建。由于仔细描述了对当前工作中的风暴浪涌陆地浪涌的陆地湿地特征的仔细描述,沿着河流,小溪和泻湖的不准确代表沿海淹没模拟的主要缺点。沿海淹没的实验模拟是对Phailin(2013)和Hudhud(2014)旋风进行的。将计算的Phailin和Hudhud的浪涌残留物与可用的潮汐仪表观察进行比较,这导致了0.06μm和0.11μm的根均方误差。模拟表现出现实的沿海淹没,与印度气象部门记录相比。然后使用模型设置,以产生由于Titli(2018)旋风的沿海淹没预测,其克里酮为48小时。天气研究和预测模型预测风量为5公里的空间分辨率用作主要迫使参数。通过评估从加拿大卫星雷达-2划分的综合孔径图像划分的模拟淹没的模拟淹没的空间一致性,验证了沿着旋转旋风的沿海淹没预测。结果清楚地表明了模型性能的可接受性,可能在旋风内预测沿海淹没进行操作预警。

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