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Hydrological Modeling in the Upper Lancang-Mekong River Basin Using Global and Regional Gridded Meteorological Re-Analyses
被引:2
|作者:
Zhang, Shixiao
[1
]
Lang, Yang
[1
]
Yang, Furong
[1
]
Qiao, Xinran
[1
]
Li, Xiuni
[1
,2
]
Gu, Yuefei
[3
]
Yi, Qi
[1
]
Luo, Lifeng
[4
,5
]
Duan, Qingyun
[6
]
机构:
[1] Yunnan Univ, Sch Earth Sci, Kunming 650050, Peoples R China
[2] Cent China Normal Univ, Coll Urban & Environm Sci, Wuhan 430079, Peoples R China
[3] Yunnan Univ, Inst Int Rivers & Ecosecur, Kunming 650050, Peoples R China
[4] Michigan State Univ, Dept Geog Environm & Spatial Sci, E Lansing, MI 48824 USA
[5] Michigan State Univ, Ctr Global Change & Earth Observat, E Lansing, MI 48824 USA
[6] Hohai Univ, Coll Hydrol & Water Resources, Nanjing 210098, Peoples R China
来源:
基金:
中国国家自然科学基金;
关键词:
CFSR;
CMADS;
meteorological variables;
hydrological simulations;
SWAT plus;
upper Lancang-Mekong River Basin (LMRB);
SENSITIVITY-ANALYSIS METHODS;
RAINFALL-RUNOFF MODELS;
CLIMATE-CHANGE;
SWAT MODEL;
INPUT DATA;
PRECIPITATION;
CALIBRATION;
STREAMFLOW;
ACCURACY;
IMPACTS;
D O I:
10.3390/w15122209
中图分类号:
X [环境科学、安全科学];
学科分类号:
08 ;
0830 ;
摘要:
Multisource meteorological re-analyses provide the most reliable forcing data for driving hydrological models to simulate streamflow. We aimed to assess different hydrological responses through hydrological modeling in the upper Lancang-Mekong River Basin (LMRB) using two gridded meteorological datasets, Climate Forecast System Re-analysis (CFSR) and the China Meteorological Assimilation Driving Datasets for the Soil and Water Assessment Tool (SWAT) model (CMADS). We selected the Pearson's correlation coefficient (R), percent bias (PBIAS), and root mean square error (RMSE) indices to compare the six meteorological variables of the two datasets. The spatial distributions of the statistical indicators in CFSR and CMADS, namely, the R, PBIAS, and RMSE values, were different. Furthermore, the soil and water assessment tool plus (SWAT+) model was used to perform hydrological modeling based on CFSR and CMADS meteorological re-analyses in the upper LMRB. The different meteorological datasets resulted in significant differences in hydrological responses, reflected by variations in the sensitive parameters and their optimal values. The differences in the calibrated optimal values for the sensitive parameters led to differences in the simulated water balance components between the CFSR- and CMADS-based SWAT+ models. These findings could help improve the understanding of the strengths and weaknesses of different meteorological re-analysis datasets and their roles in hydrological modeling.
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页数:24
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