CoastFLOOD: A High-Resolution Model for the Simulation of Coastal Inundation Due to Storm Surges

被引:8
作者
Makris, Christos [1 ]
Mallios, Zisis [1 ]
Androulidakis, Yannis [1 ]
Krestenitis, Yannis [1 ]
机构
[1] Aristotle Univ Thessaloniki, Sch Civil Engn, Div Hydraul & Environm Engn, Lab Maritime Engn & Maritime Works, Thessaloniki 54124, Greece
关键词
coastal flooding; numerical modelling; storm surge; sea level elevation; inundation maps; Manning coefficient; raster grid; DIFFERENCE WATER INDEX; SEA-LEVEL RISE; NEW-YORK-CITY; FLOOD INUNDATION; MEDITERRANEAN SEA; VULNERABILITY ASSESSMENT; HYDRODYNAMIC MODEL; VARIABILITY; IMPACT; COMPLEXITY;
D O I
10.3390/hydrology10050103
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Storm surges due to severe weather events threaten low-land littoral areas by increasing the risk of seawater inundation of coastal floodplains. In this paper, we present recent developments of a numerical modelling system for coastal inundation induced by sea level elevation due to storm surges enhanced by astronomical tides. The proposed numerical code (CoastFLOOD) performs high-resolution (5 m x 5 m) raster-based, storage-cell modelling of coastal inundation by Manning-type equations in decoupled 2-D formulation at local-scale (20 km x 20 km) lowland littoral floodplains. It is fed either by outputs of either regional-scale storm surge simulations or satellite altimetry data for the sea level anomaly. The presented case studies refer to model applications at 10 selected coastal sites of the Ionian Sea (east-central Mediterranean Sea). The implemented regular Cartesian grids (up to 5 m) are based on Digital Elevation/Surface Models (DEM/DSM) of the Hellenic Cadastre. New updated features of the model are discussed herein concerning the detailed surveying of terrain roughness and bottom friction, the expansion of Dirichlet boundary conditions for coastal currents (besides sea level), and the enhancement of wet/dry cell techniques for flood front propagation over steep water slopes. Verification of the model is performed by comparisons against satellite ocean color observations (Sentinel-2 images) and estimated flooded areas by the Normalized Difference Water Index (NDWI). The qualitative comparisons are acceptable, i.e., the modelled flooded areas contain all wet area estimations by NDWI. CoastFLOOD results are also compared to a simplified, static level, "bathtub" inundation approach with hydraulic connectivity revealing very good agreement (goodness-of-fit > 0.95). Furthermore, we show that proper treatment of bottom roughness referring to realistic Land Cover datasets provides more realistic estimations of the maximum flood extent timeframe.
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页数:44
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