Abstract

Abstract. The use of ensemble streamflow forecasts is developing in the international flood forecasting services. Ensemble streamflow forecast systems can provide more accurate forecasts and useful information about the uncertainty of the forecasts, thus improving the assessment of risks. Nevertheless, these systems, like all hydrological forecasts, suffer from errors on initialization or on meteorological data, which lead to hydrological prediction errors. This article, which is the second part of a 2-part article, concerns the impacts of initial states, improved by a streamflow assimilation system, on an ensemble streamflow prediction system over France. An assimilation system was implemented to improve the streamflow analysis of the SAFRAN-ISBA-MODCOU (SIM) hydro-meteorological suite, which initializes the ensemble streamflow forecasts at Météo-France. This assimilation system, using the Best Linear Unbiased Estimator (BLUE) and modifying the initial soil moisture states, showed an improvement of the streamflow analysis with low soil moisture increments. The final states of this suite were used to initialize the ensemble streamflow forecasts of Météo-France, which are based on the SIM model and use the European Centre for Medium-range Weather Forecasts (ECMWF) 10-day Ensemble Prediction System (EPS). Two different configurations of the assimilation system were used in this study: the first with the classical SIM model and the second using improved soil physics in ISBA. The effects of the assimilation system on the ensemble streamflow forecasts were assessed for these two configurations, and a comparison was made with the original (i.e. without data assimilation and without the improved physics) ensemble streamflow forecasts. It is shown that the assimilation system improved most of the statistical scores usually computed for the validation of ensemble predictions (RMSE, Brier Skill Score and its decomposition, Ranked Probability Skill Score, False Alarm Rate, etc.), especially for the first few days of the time range. The assimilation was slightly more efficient for small basins than for large ones.

Highlights

  • The development of meteorological ensemble prediction systems (EPSs) during recent years has allowed their use to spread into many related topics

  • The first part of this study describes the SIM hydrometeorological model used and the way ensemble streamflow predictions are set up from this system with the ECMWF (European Centre for Medium-range Weather Forecasts) EPS

  • The original system was initialized by the real-time SIManalysis suite but the two sets of improved initial states used a re-analysed SAFRAN-analysis and the version of the assimilation system with the variable state using a combination of the soil moisture of the two soil layers

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Summary

Introduction

The development of meteorological ensemble prediction systems (EPSs) during recent years has allowed their use to spread into many related topics. Several studies are developing on this topic, and aim to use past discharges in order to improve hydrological states of models. The aim of this study was to assess the effects of using initial states improved by a past discharge assimilation system as described in Thirel et al (2010a), on ensemble streamflow forecasts over France. That is why a data assimilation system using past discharges and incrementing the soil moisture states of the model was implemented in testing mode, in order to improve the hydro-meteorological analysis (Thirel et al, 2010a). The first part of this study describes the SIM hydrometeorological model used and the way ensemble streamflow predictions are set up from this system with the ECMWF (European Centre for Medium-range Weather Forecasts) EPS. A large set of statistical scores will be used to quantify the impacts of the assimilation system on the 10-day SIM-ECMWF ensemble streamflow system, first for 148 assimilated stations and for 49 independent stations

The SIM model
The meteorological EPS used
The SIM ensemble streamflow predictions
The past discharge assimilation system
Impacts of the assimilation system on the ensemble streamflow forecasts
Set-up of the experiments
Basin size study
Analysis on independent stations
Findings
Conclusions
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