Abstract

Flooding is one of the major natural hazards in the UK. Accurate flood estimation at ungauged catchment is an important component to understand and mitigate flood hazards, but still a difficult issue. This study therefore attempts to explore and improve an index flood estimation model, known as the FEH-QMED model, popular in the UK. It was developed under the assumption that the index flood of QMED, i.e., the median of the set of annual maximum (AMAX) flood data, standing for a flooding level of 2-year return period, can be explained by catchment descriptors. In this study, two fundamentals are empirically explored, including assessing reliability of the nonlinear functional impacts of the catchment descriptors on the logarithmic transformation of QMED, specified by the FEH-QMED model, and the potential to improve the model for more accurate index flood estimation, based on the flooding data of 586 gauged stations across the UK. Through a spatial additive regression analysis, we empirically find that the nonlinear impacts of the catchment descriptors in an updated FEH-QMED model appear reliable. However, spatial correlation tests including Moran’s I and Lagrange multiplier tests show that strong spatial dependence exists in the residuals of, but was not fully taken into account by, the QMED type models. We have therefore empirically established new spatial index flood estimation models by proposing spatial autoregressive models to model the impacts of the neighboring sites. Cross-validation assessments demonstrate that the suggested spatial error-based index flood model outperforms the updated FEH-QMED model with a significant improvement, which is robust in the sense of different error measures, say by a reduction of 13.8% of the mean squared error of prediction, for the UK index flood estimation.

Highlights

  • Flooding is a major natural hazard in the UK [53], with more than 5 million people living or working in flood prone areas in England and Wales alone [54]

  • The observed flood peak data are from the HiFlows-UK project, which are available at http://nrfa.ceh.ac.uk/data/search, while the data on physical catchment descriptors are from the Flood Estimation Handbook (FEH) CD-ROM 3.0, which can be accessed through the website at https://fehweb.ceh.ac.uk/

  • The median annual maximum flood (QMED) in logarithm is considered as the response variable, Y = ln(QMED), which is a function of the four predictor variables, i.e., the catchment drainage area (AREA), the average annual rainfall (SAAR), the flood attenuation by reservoirs and lakes (FARL), and the base flow index by hydrology of soil type data (BFIHOST)

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Summary

Introduction

Flooding is a major natural hazard in the UK [53], with more than 5 million people living or working in flood prone areas in England and Wales alone [54]. We find that the additive analysis confirms the non-linear effects of the catchment descriptors specified by the FEH-QMED model, while the Moran test and a spatial error analysis show that the spatial autocorrelations significantly exist in our flood data These facts lead us to propose spatial autoregressive index flood estimation models by more fully taking account of the spatial dependence, which we will demonstrate outperform the updated FEH-QMED model of [33] in improvement of prediction, which is robust in the sense of different error measures, say by a reduction of 13.8% of the mean squared error for prediction of the logarithmic QMED.

Data Source
The Flood Regionalization Procedure
The FEH-QMED Model
Methodology
Spatial Additive Analysis
Spatial Dependence and Autoregressive Analysis
Empirical Spatial Additive Assessment of the FEH-QMED Model
Empirical Tests of Spatial Autocorrelation
An Improved Index Flood Estimation
Findings
Conclusion
Full Text
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