Abstract

As runoff patterns shift with a changing climate, it is critical to effectively communicate current and future flood risks, yet existing flood hazard maps are insufficient. Modifying, extending, or updating flood inundation extents is difficult, especially over large scales, because traditional floodplain mapping approaches are data and resource intensive. Low-complexity floodplain mapping techniques are promising alternatives, but their simplistic representation of process falls short of capturing inundation patterns in all situations or settings. To address these needs and deficiencies, we formalize and extend the functionality of the Height Above Nearest Drainage (i.e., HAND) floodplain mapping approach into the probHAND model by incorporating an uncertainty analysis. With publicly available datasets, the probHAND model can produce probabilistic floodplain maps for large areas relatively rapidly. We describe the modeling approach and then provide an example application in the Lake Champlain Basin, Vermont, USA. Uncertainties translate to on-the-ground changes to inundated areas, or floodplain widths, in the study area by an average of 40%. We found that the spatial extent of probable inundation captured the distribution of observed and modeled flood extents well, suggesting that low-complexity models may be sufficient for representing inundation extents in support of flood risk and conservation mapping applications, especially when uncertainties in parameter inputs and process simplifications are accounted for. To improve the accuracy of flood hazard datasets, we recommend investing limited resources in accurate topographic datasets and improved flood frequency analyses. Such investments will have the greatest impact on decreasing model output variability, therefore increasing the certainty of flood inundation extents.

Highlights

  • Runoff and streamflow patterns are shifting as a result of climate change [1,2]

  • Our results demonstrate the value of simple probabilistic floodplain mapping approaches and have important implications for model-based flood risk management and conservation

  • We evaluated the integrity of probHAND model outputs using predictions from a 1D hydraulic model

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Summary

Introduction

Runoff and streamflow patterns are shifting as a result of climate change [1,2]. Additional funding was provided to RMD by the Gund Institute for Environment at the University of Vermont (www.uvm.edu/gund). The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript

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