Journal cover Journal topic
Hydrology and Earth System Sciences An interactive open-access journal of the European Geosciences Union
Hydrol. Earth Syst. Sci., 13, 2221-2231, 2009
© Author(s) 2009. This work is distributed
under the Creative Commons Attribution 3.0 License.
25 Nov 2009
An evaluation of the Canadian global meteorological ensemble prediction system for short-term hydrological forecasting
J. A. Velázquez1, T. Petit1, A. Lavoie1, M.-A. Boucher1, R. Turcotte2, V. Fortin3, and F. Anctil1 1Chaire de recherche EDS en prévisions et actions hydrologiques, Université Laval, Québec, Canada
2Centre d'expertise hydrique du Québec, Québec, Canada
3Recherche en prévision numérique environnementale, Environnement Canada, Montréal, Canada
Abstract. Hydrological forecasting consists in the assessment of future streamflow. Current deterministic forecasts do not give any information concerning the uncertainty, which might be limiting in a decision-making process. Ensemble forecasts are expected to fill this gap.

In July 2007, the Meteorological Service of Canada has improved its ensemble prediction system, which has been operational since 1998. It uses the GEM model to generate a 20-member ensemble on a 100 km grid, at mid-latitudes. This improved system is used for the first time for hydrological ensemble predictions. Five watersheds in Quebec (Canada) are studied: Chaudière, Châteauguay, Du Nord, Kénogami and Du Lièvre. An interesting 17-day rainfall event has been selected in October 2007. Forecasts are produced in a 3 h time step for a 3-day forecast horizon. The deterministic forecast is also available and it is compared with the ensemble ones. In order to correct the bias of the ensemble, an updating procedure has been applied to the output data. Results showed that ensemble forecasts are more skilful than the deterministic ones, as measured by the Continuous Ranked Probability Score (CRPS), especially for 72 h forecasts. However, the hydrological ensemble forecasts are under dispersed: a situation that improves with the increasing length of the prediction horizons. We conjecture that this is due in part to the fact that uncertainty in the initial conditions of the hydrological model is not taken into account.

Citation: Velázquez, J. A., Petit, T., Lavoie, A., Boucher, M.-A., Turcotte, R., Fortin, V., and Anctil, F.: An evaluation of the Canadian global meteorological ensemble prediction system for short-term hydrological forecasting, Hydrol. Earth Syst. Sci., 13, 2221-2231, doi:10.5194/hess-13-2221-2009, 2009.
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