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Modelling coastal flood vulnerability: Does spatially-distributed friction improve the prediction of flood extent?

机译:对沿海洪灾脆弱性进行建模:空间分布摩擦是否可以改善对洪灾程度的预测?

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This paper examines whether the application of spatially-distributed versus static friction in hydrodynamic modelling increases the accuracy of predicted coastal flood extent using Pigeon Point, southwest Tobago, as a case in point. A two-dimensional hydrodynamic flood model is created from acquired and surveyed bathymetric, topographic and tidal data via the LISFLOOD-FP model code. Using a Landsat 8 image of the study area, a Maximum Likelihood (ML) supervised classification was performed to distinguish different land cover classes within the study site. The classified Landsat 8 image was further processed by assigning friction values to each land cover class to create a spatially-distributed friction file in ASCII format for use in LISFLOOD-FP. Using the flood model developed, simultaneous simulations were performed to assess the impact of storm surges (varying levels) on coastal flood extent at Pigeon Point utilising a static friction value, which broadly defined the area (i.e., 0.02), and the spatially-distributed friction file generated. Model outputs were compared to determine the extent of difference in flood prediction obtained from the application of static versus spatially-distributed friction through a Geographic Information System (GIS) based analysis. The flood model developed was subsequently applied to simulate an observed spring tide event using both static and spatially-distributed friction value(s) defined and model performance in each case was evaluated using the Root Mean Squared Error (RMSE) approach. Collated results indicated that using spatially-distributed over static friction do not increase accuracy of predicted coastal inundation extent, nor improve model performance. However, it appears to provide more insight on flood timings, which can be useful for coastal management. (C) 2015 Elsevier Ltd. All rights reserved.
机译:本文以多巴哥西南部的鸽角为例,研究在水动力模型中应用空间分布与静摩擦之间的关系是否可以提高预测的沿海洪灾程度的准确性。通过LISFLOOD-FP模型代码,从采集和调查的测深,地形和潮汐数据中创建二维水力洪水模型。使用研究区域的Landsat 8图像,进行了最大似然(ML)监督分类,以区分研究地点内的不同土地覆盖类别。通过为每个土地覆盖类别分配摩擦值来进一步处理分类的Landsat 8图像,以创建用于ASCII格式的空间分布摩擦文件,以供LISFLOOD-FP使用。使用开发的洪水模型,同时进行模拟,以评估风暴潮(水平变化)对鸽子点沿海洪灾程度的影响,利用静摩擦值广义地定义了面积(即0.02)和空间分布生成摩擦文件。通过基于地理信息系统(GIS)的分析,比较了模型输出以确定通过应用静摩擦与空间分布摩擦获得的洪水预测差异的程度。随后使用定义的静态和空间分布摩擦值将开发的洪水模型应用于模拟观测到的潮汐事件,并使用均方根误差(RMSE)方法评估每种情况下的模型性能。整理的结果表明,使用空间分布的静摩擦不会提高预测的沿海淹没程度的准确性,也不会提高模型的性能。但是,它似乎可以提供更多有关洪水时间的信息,这对于沿海地区的管理很有用。 (C)2015 Elsevier Ltd.保留所有权利。

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