On the incidence of meteorological and hydrological processors: Effect of resolution, sharpness and reliability of hydrological ensemble forecasts

被引:15
作者
Abaza, Mabrouk [1 ]
Anctil, Francois [1 ]
Fortin, Vincent [2 ]
Perreault, Luc [3 ]
机构
[1] Univ Laval, Dept Civil & Water Engn, Pavillon Adrien Pouliot,1065,Ave Med, Quebec City, PQ, Canada
[2] Environm & Climate Change Canada, 2121,Route Transcanadienne Dorval, Montreal, PQ H9P 1J3, Canada
[3] Hydro Quebec Res Inst, 1800,Blvd Lionel Boulet, Varennes, PQ J3X 1S1, Canada
基金
加拿大自然科学与工程研究理事会;
关键词
Meteorological processor; Hydrological processor; Resolution; Sharpness; Reliability; Performance; MODEL OUTPUT STATISTICS; CLIMATE-CHANGE; PRECIPITATION FORECASTS; DATA ASSIMILATION; SCORING RULES; PREDICTION; UNCERTAINTY; IMPROVEMENT; RAINFALL; IMPACT;
D O I
10.1016/j.jhydrol.2017.10.038
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
Meteorological and hydrological ensemble prediction systems are imperfect. Their outputs could often be improved through the use of a statistical processor, opening up the question of the necessity of using both processors (meteorological and hydrological), only one of them, or none. This experiment compares the predictive distributions from four hydrological ensemble prediction systems (H-EPS) utilising the Ensemble Kalman filter (EnKF) probabilistic sequential data assimilation scheme. They differ in the inclusion or not of the Distribution Based Scaling (DBS) method for post-processing meteorological forecasts and the ensemble Bayesian Model Averaging (ensemble BMA) method for hydrological forecast post-processing. The experiment is implemented on three large watersheds and relies on the combination of two meteorological reforecast products: the 4-member Canadian reforecasts from the Canadian Centre for Meteorological and Environmental Prediction (CCMEP) and the 10-member American reforecasts from the National Oceanic and Atmospheric Administration (NOAA), leading to 14 members at each time step. Results show that all four tested H-EPS lead to resolution and sharpness values that are quite similar, with an advantage to DBS + EnKF. The ensemble BMA is unable to compensate for any bias left in the precipitation ensemble forecasts. On the other hand, it succeeds in calibrating ensemble members that are otherwise under-dispersed. If reliability is preferred over resolution and sharpness, DBS + EnKF + ensemble BMA performs best, making use of both processors in the H-EPS system. Conversely, for enhanced resolution and sharpness, DBS is the preferred method. Crown Copyright (C) 2017 Published by Elsevier B.V. All rights reserved.
引用
收藏
页码:371 / 384
页数:14
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