An integrated uncertainty and ensemble-based data assimilation approach for improved operational streamflow predictions

被引:26
作者
He, M. [1 ]
Hogue, T. S. [1 ]
Margulis, S. A. [1 ]
Franz, K. J. [2 ]
机构
[1] Univ Calif Los Angeles, Dept Civil & Environm Engn, Los Angeles, CA 90024 USA
[2] Iowa State Univ, Dept Geol & Atmospher Sci, Ames, IA USA
关键词
SEQUENTIAL DATA ASSIMILATION; CONCEPTUAL HYDROLOGIC MODEL; 1997 FIELD EXPERIMENT; SNOW-COVERED AREA; PARAMETER-ESTIMATION; VERIFICATION; STATE; CALIBRATION; FORECAST; PRECIPITATION;
D O I
10.5194/hess-16-815-2012
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The current study proposes an integrated uncertainty and ensemble-based data assimilation framework (ICEA) and evaluates its viability in providing operational streamflow predictions via assimilating snow water equivalent (SWE) data. This step-wise framework applies a parameter uncertainty analysis algorithm (ISURF) to identify the uncertainty structure of sensitive model parameters, which is subsequently formulated into an Ensemble Kalman Filter (EnKF) to generate updated snow states for streamflow prediction. The framework is coupled to the US National Weather Service (NWS) snow and rainfall-runoff models. Its applicability is demonstrated for an operational basin of a western River Forecast Center (RFC) of the NWS. Performance of the framework is evaluated against existing operational baseline (RFC predictions), the stand-alone ISURF and the stand-alone EnKF. Results indicate that the ensemble-mean prediction of ICEA considerably outperforms predictions from the other three scenarios investigated, particularly in the context of predicting high flows (top 5th percentile). The ICEA streamflow ensemble predictions capture the variability of the observed streamflow well, however the ensemble is not wide enough to consistently contain the range of streamflow observations in the study basin. Our findings indicate that the ICEA has the potential to supplement the current operational (deterministic) forecasting method in terms of providing improved single-valued (e.g., ensemble mean) streamflow predictions as well as meaningful ensemble predictions.
引用
收藏
页码:815 / 831
页数:17
相关论文
共 73 条
[31]  
Gelman A., 1992, Statist. Sci., V7, P457
[32]  
He M., 2010, Data assimilation in watershed models for improved hydrologic forecasting
[33]   Corruption of parameter behavior and regionalization by model and forcing data errors: A Bayesian example using the SNOW17 model [J].
He, Minxue ;
Hogue, Terri S. ;
Franz, Kristie J. ;
Margulis, Steven A. ;
Vrugt, Jasper A. .
WATER RESOURCES RESEARCH, 2011, 47
[34]   Characterizing parameter sensitivity and uncertainty for a snow model across hydroclimatic regimes [J].
He, Minxue ;
Hogue, Terri S. ;
Franz, Kristie J. ;
Margulis, Steven A. ;
Vrugt, Jasper A. .
ADVANCES IN WATER RESOURCES, 2011, 34 (01) :114-127
[35]   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
[36]  
Hogue TS, 2000, J HYDROMETEOROL, V1, P524, DOI 10.1175/1525-7541(2000)001<0524:AMACSF>2.0.CO
[37]  
2
[38]  
HORNBERGER GM, 1981, J ENVIRON MANAGE, V12, P7
[39]   Numerical investigation of the impact of uncertainties in satellite rainfall estimation and land surface model parameters on simulation of soil moisture [J].
Hossain, F ;
Anagnostou, EN .
ADVANCES IN WATER RESOURCES, 2005, 28 (12) :1336-1350
[40]  
Kavetski D., 2002, CALIBRATION WATERSHE, P49, DOI [10.1029/WS006p0049, DOI 10.1029/WS006P0049]