Real-time data assimilation for operational ensemble streamflow forecasting

被引:139
作者
Vrugt, Jasper A.
Gupta, Hoshin V.
Nuallain, Breanndan O.
机构
[1] Los Alamos Natl Lab, Div Earth & Environm Sci, Los Alamos, NM 87544 USA
[2] Univ Arizona, Dept Hydrol & Water Resources, Tucson, AZ 85721 USA
[3] Univ Amsterdam, Dept Computat Sci, Amsterdam, Netherlands
[4] Univ Amsterdam, Dept Phys Geog & Soil Sci, Amsterdam, Netherlands
关键词
D O I
10.1175/JHM504.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Operational flood forecasting requires that accurate estimates of the uncertainty associated with model-generated streamflow forecasts be provided along with the probable flow levels. This paper demonstrates a stochastic ensemble implementation of the Sacramento model used routinely by the National Weather Service for deterministic streamflow forecasting. The approach, the simultaneous optimization and data assimilation method ( SODA), uses an ensemble Kalman filter (EnKF) for recursive state estimation allowing for treatment of streamflow data error, model structural error, and parameter uncertainty, while enabling implementation of the Sacramento model without major modification to its current structural form. Model parameters are estimated in batch using the shuffled complex evolution metropolis stochastic-ensemble optimization approach (SCEM-UA). The SODA approach was implemented using parallel computing to handle the increased computational requirements. Studies using data from the Leaf River, Mississippi, indicate that forecast performance improvements on the order of 30% to 50% can be realized even with a suboptimal implementation of the filter. Further, the SODA parameter estimates appear to be less biased, which may increase the prospects for finding useful regionalization relationships.
引用
收藏
页码:548 / 565
页数:18
相关论文
共 76 条
[31]  
GUPTA HV, 2003, WATER SCI APPL SERIE, V6, P113
[32]   THE RELATIONSHIP BETWEEN DATA AND THE PRECISION OF PARAMETER ESTIMATES OF HYDROLOGIC-MODELS [J].
GUPTA, VK ;
SOROOSHIAN, S .
JOURNAL OF HYDROLOGY, 1985, 81 (1-2) :57-77
[33]  
HALL P, 1990, BIOMETRIKA, V77, P521, DOI 10.1093/biomet/77.3.521
[34]   A 'User-Friendly' approach to parameter estimation in hydrologic models [J].
Hogue, TS ;
Gupta, H ;
Sorooshian, S .
JOURNAL OF HYDROLOGY, 2006, 320 (1-2) :202-217
[35]  
Hogue TS, 2000, J HYDROMETEOROL, V1, P524, DOI 10.1175/1525-7541(2000)001<0524:AMACSF>2.0.CO
[36]  
2
[37]   Self-organizing linear output map (SOLO): An artificial neural network suitable for hydrologic modeling and analysis [J].
Hsu, KL ;
Gupta, HV ;
Gao, XG ;
Sorooshian, S ;
Imam, B .
WATER RESOURCES RESEARCH, 2002, 38 (12)
[38]   HOW MUCH COMPLEXITY IS WARRANTED IN A RAINFALL-RUNOFF MODEL [J].
JAKEMAN, AJ ;
HORNBERGER, GM .
WATER RESOURCES RESEARCH, 1993, 29 (08) :2637-2649
[39]  
Kalman RE., 1960, J BASIC ENG, V82, P35, DOI DOI 10.1115/1.3662552
[40]  
Kavetski D., 2002, CALIBRATION WATERSHE, P49, DOI [DOI 10.1029/WS006P0049, 10.1029/WS006p0049]