TY - JOUR
T1 - A toy model for monthly river flow forecasting
AU - Zeng, Xubin
AU - Kiviat, Kira L.
AU - Sakaguchi, Koichi
AU - Mahmoud, Alaa M.A.
N1 - Funding Information:
This work was supported by NASA (NNX09A021G), NSF (AGS-0944101), and DOE (DE-SC0006773). The river flow data are obtained from http://www.cgd.ucar.edu/cas/catalog/ , while the precipitation data from http://badc.nerc.ac.uk . Dr. Aihui Wang is thanked for providing the river basin averaged monthly precipitation.
PY - 2012/7/25
Y1 - 2012/7/25
N2 - River flow forecasting depends on land-atmosphere coupled processes, and is relevant to hydrological applications and land-ocean coupling. A toy model is developed here for monthly river flow forecasting using the river flow and river basin averaged precipitation in prior month. Model coefficients are calibrated for each month using historical data. The toy model is based on water balance, easy to use and reproduce, and robust to calibrate with a short period of data. For five major rivers in the world, its results agree with observations very well. Its prediction uncertainty can be quantified using the model's error statistics or using a dynamic approach, but not by the dispersion of 10,000 ensemble members with different sets of coefficients in the model. Its results are much better than those from a physically based land model even after the mean bias correction. The toy model and a standard neural network available from the MATLAB give similar results, but the latter is more sensitive to the length of calibration period. For the monthly prediction of river flow with a strong seasonal cycle, a modified Nash-Sutcliffe coefficient of efficiency is introduced and is found to be more reliable in model evaluations than the original coefficient of efficiency or the correlation coefficient.
AB - River flow forecasting depends on land-atmosphere coupled processes, and is relevant to hydrological applications and land-ocean coupling. A toy model is developed here for monthly river flow forecasting using the river flow and river basin averaged precipitation in prior month. Model coefficients are calibrated for each month using historical data. The toy model is based on water balance, easy to use and reproduce, and robust to calibrate with a short period of data. For five major rivers in the world, its results agree with observations very well. Its prediction uncertainty can be quantified using the model's error statistics or using a dynamic approach, but not by the dispersion of 10,000 ensemble members with different sets of coefficients in the model. Its results are much better than those from a physically based land model even after the mean bias correction. The toy model and a standard neural network available from the MATLAB give similar results, but the latter is more sensitive to the length of calibration period. For the monthly prediction of river flow with a strong seasonal cycle, a modified Nash-Sutcliffe coefficient of efficiency is introduced and is found to be more reliable in model evaluations than the original coefficient of efficiency or the correlation coefficient.
KW - Modified Nash-Sutcliffe coefficient of efficiency
KW - Neural network
KW - River flow forecasting
KW - Uncertainty quantification
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U2 - 10.1016/j.jhydrol.2012.05.053
DO - 10.1016/j.jhydrol.2012.05.053
M3 - Article
AN - SCOPUS:84863091632
SN - 0022-1694
VL - 452-453
SP - 226
EP - 231
JO - Journal of Hydrology
JF - Journal of Hydrology
ER -