Abstract

Abstract. A large effort has been made over the past 10 years to promote the operational use of probabilistic or ensemble streamflow forecasts. Numerous studies have shown that ensemble forecasts are of higher quality than deterministic ones. Many studies also conclude that decisions based on ensemble rather than deterministic forecasts lead to better decisions in the context of flood mitigation. Hence, it is believed that ensemble forecasts possess a greater economic and social value for both decision makers and the general population. However, the vast majority of, if not all, existing hydro-economic studies rely on a cost–loss ratio framework that assumes a risk-neutral decision maker. To overcome this important flaw, this study borrows from economics and evaluates the economic value of early warning flood systems using the well-known Constant Absolute Risk Aversion (CARA) utility function, which explicitly accounts for the level of risk aversion of the decision maker. This new framework allows for the full exploitation of the information related to a forecasts' uncertainty, making it especially suited for the economic assessment of ensemble or probabilistic forecasts. Rather than comparing deterministic and ensemble forecasts, this study focuses on comparing different types of ensemble forecasts. There are multiple ways of assessing and representing forecast uncertainty. Consequently, there exist many different means of building an ensemble forecasting system for future streamflow. One such possibility is to dress deterministic forecasts using the statistics of past error forecasts. Such dressing methods are popular among operational agencies because of their simplicity and intuitiveness. Another approach is the use of ensemble meteorological forecasts for precipitation and temperature, which are then provided as inputs to one or many hydrological model(s). In this study, three concurrent ensemble streamflow forecasting systems are compared: simple statistically dressed deterministic forecasts, forecasts based on meteorological ensembles, and a variant of the latter that also includes an estimation of state variable uncertainty. This comparison takes place for the Montmorency River, a small flood-prone watershed in southern central Quebec, Canada. The assessment of forecasts is performed for lead times of 1 to 5 days, both in terms of forecasts' quality (relative to the corresponding record of observations) and in terms of economic value, using the new proposed framework based on the CARA utility function. It is found that the economic value of a forecast for a risk-averse decision maker is closely linked to the forecast reliability in predicting the upper tail of the streamflow distribution. Hence, post-processing forecasts to avoid over-forecasting could help improve both the quality and the value of forecasts.

Highlights

  • More than 15 years after its advocation by (Krzysztofowicz, 2001) and more than a decade after the creation of the Hydrologic Ensemble Prediction EXperiment (HEPEX) commu-Published by Copernicus Publications on behalf of the European Geosciences Union.S

  • The streamflow forecasts based on meteorological ensembles have better CRPS than dressed deterministic forecasts, but their value according to the Constant Absolute Risk Aversion (CARA) utility function is lower

  • The purpose of this study is to set the basis of an alternative framework to replace the cost–loss ratio in economic assessment of early warning flood forecasting systems

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Summary

Introduction

More than 15 years after its advocation by (Krzysztofowicz, 2001) and more than a decade after the creation of the Hydrologic Ensemble Prediction EXperiment (HEPEX) commu-S. (Beven, 2016) distinguishes aleatory uncertainty, which originates from data only and possesses stationary statistical characteristics, from various types of epistemic uncertainties. As discussed in (Juston et al, 2013), uncertainty in hydrological forecasting mainly originates from data and models (atmospheric and hydrologic). The most important sources of uncertainty in short-term hydrological forecasting are structural uncertainty (choice of a particular hydrological model structure), state variable uncertainty and parameter uncertainty, which are both linked to the availability and quality of hydro-meteorological data, and meteorological forecast uncertainty. The latter gains in importance gradually as the forecasting horizon increases

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