2018
DOI: 10.1111/jfr3.12508
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A partition of the combined impacts of socioeconomic development and climate variation on economic risks of riverine floods

Abstract: Nonstationarities in both climate and socioeconomic systems play a role in flood risk. Based on a data‐driven case study in an urbanised watershed subjected to nonstationary factors in climate (rain, snow, and rain on snow) and socioeconomic conditions (e.g., built environment market changes), a multiscale, multimodel approach was adopted to develop local‐scale flood hazard predictions and an analytical framework was developed to quantify the associated flood risk. The case study shows that socioeconomic devel… Show more

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“…Mapping inundation in a timely and accurate manner for the consequential floods caused by major weather events is never easy and depends on a cascading chain of model structures with uncertainties accumulated at every node. A typical model chain usually takes an ensemble of numerical weather predictions (NWPs) as the boundary conditions to force a hydrologic model to simulate rainfall-runoff processes over the catchment and then adopts the simulated overland runoff as the successive boundary conditions to drive a hydraulic channel routing model to predict streamflow [1][2][3]. The chain of models coupled at various scales makes up the backbone of the current continental-scale and global-scale streamflow forecasting platforms, such as the European Flood Forecasting System (EFFS), the U.S. National Oceanic and Atmospheric Administration's National Water Model (NWM), or the Global Flood Awareness System (GloFAS).…”
Section: Introductionmentioning
confidence: 99%
“…Mapping inundation in a timely and accurate manner for the consequential floods caused by major weather events is never easy and depends on a cascading chain of model structures with uncertainties accumulated at every node. A typical model chain usually takes an ensemble of numerical weather predictions (NWPs) as the boundary conditions to force a hydrologic model to simulate rainfall-runoff processes over the catchment and then adopts the simulated overland runoff as the successive boundary conditions to drive a hydraulic channel routing model to predict streamflow [1][2][3]. The chain of models coupled at various scales makes up the backbone of the current continental-scale and global-scale streamflow forecasting platforms, such as the European Flood Forecasting System (EFFS), the U.S. National Oceanic and Atmospheric Administration's National Water Model (NWM), or the Global Flood Awareness System (GloFAS).…”
Section: Introductionmentioning
confidence: 99%