2018
DOI: 10.1007/s11069-018-3462-1
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An integrated 1D–2D hydraulic modelling approach to assess the sensitivity of a coastal region to compound flooding hazard under climate change

Abstract: Coastal regions are dynamic areas that often lie at the junction of different natural hazards. Extreme events such as storm surges and high precipitation are significant sources of concern for flood management. As climatic changes and sea-level rise put further pressure on these vulnerable systems, there is a need for a better understanding of the implications of compounding hazards. Recent computational advances in hydraulic modelling offer new opportunities to support decision-making and adaptation. Our rese… Show more

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Cited by 84 publications
(53 citation statements)
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“…Since 1970, considerable efforts have been made in order to improve the capabilities and functionalities of this technique. Recent computational advances in hydraulic modeling offer new opportunities to support decision-making and adaptation [49]. The applicability of streamflow models have proved efficient in flood hazard and risk mapping studies [50,51], real time flood forecasting [52], and in remodeling past flood events [53].…”
Section: State-of-the-artmentioning
confidence: 99%
“…Since 1970, considerable efforts have been made in order to improve the capabilities and functionalities of this technique. Recent computational advances in hydraulic modeling offer new opportunities to support decision-making and adaptation [49]. The applicability of streamflow models have proved efficient in flood hazard and risk mapping studies [50,51], real time flood forecasting [52], and in remodeling past flood events [53].…”
Section: State-of-the-artmentioning
confidence: 99%
“…For real-time simulations and forecasts, faster run times, and data assimilation are required to provide reliable results [21]. Recent advances in global and continental hydrological models have shown very promising results thus far, which have provided critical information regarding surface runoff, streamflow, soil moisture, soil infiltration and evapotranspiration [22][23][24][25][26][27][28]. One example is the application of the Coupled Routing and Excess Storage model embedded within the Ensemble Framework for Flash Flood Forecasting (CREST-EF5) framework [15,29,30].…”
mentioning
confidence: 99%
“…‘Probability of Flooding from River and Sea’ datasets were obtained from the Environment Agency (). Despite the historical tendency for East Coast coastal and fluvial flooding to occur independently, the concurrent river and sea flood scenarios represent the effects of ‘tide‐locking’, where high‐tide prevents river‐flow drainage, and ‘backwater’, where high water levels at the river mouth propagate upstream and exacerbate river discharge, which is possible to occur in regions such as the Broads river catchment which contains a low topographic gradient and tidal rivers (Environment Agency, ; Ikeuchi et al, ; Pasquier, He, Hooton, Goulden, & Hiscock, ). This spatial dataset, consisting of 50 m × 50 m grid cells, presents the chance of coastal and fluvial flooding in terms of high (greater than 1 in 30 year; Annual Exceedance Probability [AEP] of 3.33%), medium (between 1 in 30 year and 1 in 100 year; AEP between 3.33% and 1%), and low (between 1 in 100 year and 1 in 1000 year; AEP between 1% and 0.1%) flood risk probability, while taking into account the presence of current flood defences (Environment Agency, ).…”
Section: Methodsmentioning
confidence: 99%