Abstract

Across the globe, climate change is projected to affect the quantity, quality, and timing of freshwater availability. In western North America, there has been a shift toward earlier spring runoff and more winter precipitation as rain. This raises questions about the need for increased water storage to mitigate both floods and droughts. Some water managers have identified natural storage structures as valuable tools for increasing resiliency to these climate change impacts. However, identifying adequate sites and quantifying the storage potential of natural structures is a key challenge. This study addresses the need for a method for identifying and estimating floodplain water storage capacity in a manner that can be used by water planners through the development of a model that uses open-source geospatial data. This model was used to identify and estimate the storage capacity of a 0.33 km2 floodplain segment in eastern Montana, USA. The result is a range of storage capacities under eight natural water storage conditions, ranging from 900 m3 for small floods to 321,300 m3 for large floods. Incorporating additional hydraulic inputs, stakeholder needs, and stakeholder perceptions of natural storage into this process can help address more complex questions about using natural storage structures as ecosystem-based climate change adaptation strategies.

Highlights

  • Research in western North American climatology projects shifts in the timing of stream runoff and peak streamflow linked to increasing winter rain and declining snowpack resulting from anthropogenic climate warming [1,2]

  • The storage quantification method introduced in this paper produced a wide range of storage potentials that were most sensitive to changing α values

  • When simulating storage potential for potentials that were most sensitive to changing α values

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Summary

Introduction

Research in western North American climatology projects shifts in the timing of stream runoff and peak streamflow linked to increasing winter rain and declining snowpack resulting from anthropogenic climate warming [1,2]. Recognizing the role that natural structures (e.g., wetlands and floodplains) play in slowing runoff and promoting groundwater recharge (i.e., natural water storage), resource managers have called for the development of a project that identifies potential natural storage sites and quantifies their storage potential for the purposes of storing and retaining water for the benefit of people and ecosystems. This study develops a model for quantifying the storage capacity of natural storage systems (e.g., floodplains and wetlands) using geospatial tools rather than strictly hydrologic programs or models. The goal of this model is to preliminarily identify

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