Abstract

Abstract. Riverine flood hazard is the consequence of meteorological drivers, primarily precipitation, hydrological processes and the interaction of floodwaters with the floodplain landscape. Modeling this can be particularly challenging because of the multiple steps and differing spatial scales involved in the varying processes. As the climate modeling community increases their focus on the risks associated with climate change, it is important to translate the meteorological drivers into relevant hazard estimates. This is especially important for the climate attribution and climate projection communities. Current climate change assessments of flood risk typically neglect key processes, and instead of explicitly modeling flood inundation, they commonly use precipitation or river flow as proxies for flood hazard. This is due to the complexity and uncertainties of model cascades and the computational cost of flood inundation modeling. Here, we lay out a clear methodology for taking meteorological drivers, e.g., from observations or climate models, through to high-resolution (∼90 m) river flooding (fluvial) hazards. Thus, this framework is designed to be an accessible, computationally efficient tool using freely available data to enable greater uptake of this type of modeling. The meteorological inputs (precipitation and air temperature) are transformed through a series of modeling steps to yield, in turn, surface runoff, river flow, and flood inundation. We explore uncertainties at different modeling steps. The flood inundation estimates can then be related to impacts felt at community and household levels to determine exposure and risks from flood events. The approach uses global data sets and thus can be applied anywhere in the world, but we use the Brahmaputra River in Bangladesh as a case study in order to demonstrate the necessary steps in our hazard framework. This framework is designed to be driven by meteorology from observational data sets or climate model output. In this study, only observations are used to drive the models, so climate changes are not assessed. However, by comparing current and future simulated climates, this framework can also be used to assess impacts of climate change.

Highlights

  • Flooding is a natural phenomenon which is a part of the lives of many people around the world

  • We introduce here a new model framework which allows simulation of high-resolution flood inundation based on meteorological inputs that could come from either observations or climate models

  • FUSE is a lumped hydrological model which parameterizes the varied hydrological processes which occur within each grid cell

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Summary

Introduction

Flooding is a natural phenomenon which is a part of the lives of many people around the world. This is informative with regards to the chance of a river flooding somewhere but not for estimating the risk of flooding to specific properties, which can only be done using flood inundation models Because of these considerations, a global modeling framework that produces a cascade from meteorological information of a precipitation event through to hydrological modeling and high-resolution flood inundation modeling steps is very valuable. We propose a method for modeling each of the key steps using global, publicly available data sets in a consistent manner This allows the production of flood inundation simulations anywhere in the world at high resolution (up to 90 m), even where there are sparse observations of precipitation and river flows.

Meteorological input data sets
Generating the river network
Coarsening river network
Runoff modeling
FUSE parameter regionalization
River routing modeling
Flood inundation modeling
New LISFLOOD-FP features for this study
Input data sets
Estimating river bank elevations from the DEM
Identifying river widths
Boundary conditions at edge of domain
Inflows
Evaluation of FUSE parameter regionalization
Evaluation of routed streamflow in Ganges–Brahmaputra–Meghna
Evaluation of flood inundation in Ganges–Brahmaputra–Meghna
10 Conclusions
Full Text
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