Abstract

Abstract. Flood safety is of the utmost concern for water resources management agencies charged with operating and maintaining reservoir systems. Risk evaluations guide design of infrastructure alterations or lead to potential changes in operations. Changes in climate may change the risk due to floods and therefore decisions to alter infrastructure with a life span of decades or longer may benefit from the use of climate projections as opposed to use of only historical observations. This manuscript presents a set of methods meant to support flood frequency evaluation based on current downscaled climate projections and the potential implications of changing flood risk on how evaluations are made. Methods are demonstrated in four case study basins: the Boise River above Lucky Peak Dam, the San Joaquin River above Friant Dam, the James River above Jamestown Dam, and the Gunnison River above Blue Mesa Dam. The analytical design includes three core elements: (1) a rationale for selecting climate projections to represent available climate projections; (2) generation of runoff projections consistent with climate projections using a process-based hydrologic model and temporal disaggregation of monthly downscaled climate projections into 6-h weather forcings required by the hydrologic model; and (3) analysis of flood frequency distributions based on runoff projection results. In addition to demonstrating the methodology, this paper also presents method choices under each analytical element, and the resulting implications to how flood frequencies are evaluated. The methods used reproduce the antecedent calibration period well. The approach results in a unidirectional shift in modeled flood magnitudes. The comparison between an expanding retrospective (current paradigm for flood frequency estimation) and a lookahead flood frequency approach indicate potential for significant biases in flood frequency estimation.

Highlights

  • The design and safety assessment of large dams in the western United States requires estimates of flood frequency

  • One of the inputs into the Sacramento Soil Moisture Accounting (SAC-SMA) model is potential evapotranspiration (PET) and PET may be altered in a changing climate, the value was not altered as part of this study

  • A set of methods have been developed and presented that allow for the estimation of flood potential given a set of climate projections

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Summary

Introduction

The design and safety assessment of large dams in the western United States requires estimates of flood frequency. Raff et al.: A framework for assessing flood frequency climate, and given how flood risks are generated from the observed record of the past, it may be prudent to include information that describes the flood potential of the past and of the future. Released in 1982, Bulletin 17-B provides guidance for observational data treatment and parameter estimation for flood frequency distributions (IACWD, 1982). The process used in Bulletin 17-B assumes many things such as that the annual maximum floods are independent samples from a general population This idea that information from the past is a good indication of current potential or future potential is called a stationarity assumption. To evaluate the physical response to a changing climate there remains limited guidance on how to incorporate climate projection data into a framework for flood hazard assessment In this manuscript methods to address this gap in planning capabilities are introduced. The simulated annual maximum discharges were considered in the context of estimating flood risk through flood frequency analyses (Sect. 2.6)

Basin selection
Hydrologic tool
Climate projections data
Projection selection
Weather generation
Hydrologic hazard assessment
Weather generation for evaluating flood potential
Evaluation of flood potential by lookahead
Uncertainties
Conclusions
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