Large-scale hydrologic and hydrodynamic modeling of the Amazon River basin

被引:302
作者
Dias de Paiva, Rodrigo Cauduro [1 ,2 ]
Buarque, Diogo Costa [1 ]
Collischonn, Walter [1 ]
Bonnet, Marie-Paule [2 ]
Frappart, Frederic [2 ]
Calmant, Stephane [3 ]
Bulhoes Mendes, Carlos Andre [1 ]
机构
[1] Univ Fed Rio Grande do Sul, Inst Pesquisas Hidraul, BR-91501970 Porto Alegre, RS, Brazil
[2] Univ Toulouse 3, OMP, CNRS, Geosci Environm Toulouse UMR 5563,IRD,UPS, F-31062 Toulouse, France
[3] Univ Toulouse 3, OMP, CNRS,CNES,UPS, Lab Etud Geophysiqueet Oceanog Sci,UMR 5566,IRD, F-31062 Toulouse, France
关键词
WATER STORAGE; VARIABILITY; INUNDATION; VEGETATION; WETLAND; DEM;
D O I
10.1002/wrcr.20067
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
In this paper, a hydrologic/hydrodynamic modeling of the Amazon River basin is presented using the MGB-IPH model with a validation using remotely sensed observations. Moreover, the sources of model errors by means of the validation and sensitivity tests are investigated, and the physical functioning of the Amazon basin is also explored. The MGB-IPH is a physically based model resolving all land hydrological processes and here using a full 1-D river hydrodynamic module with a simple floodplain storage model. River-floodplain geometry parameters were extracted from the SRTM digital elevation model, and the model was forced using satellite-derived rainfall from TRMM3B42. Model results agree with observed in situ daily river discharges and water levels and with three complementary satellite-based products: (1) water levels derived from ENVISAT altimetry data; (2) a global data set of monthly inundation extent; and (3) monthly terrestrial water storage (TWS) anomalies derived from the Gravity Recovery and Climate Experimental mission. However, the model is sensitive to precipitation forcing and river-floodplain parameters. Most of the errors occur in westerly regions, possibly due to the poor quality of TRMM 3B42 rainfall data set in these mountainous and/or poorly monitored areas. In addition, uncertainty in river-floodplain geometry causes errors in simulated water levels and inundation extent, suggesting the need for improvement of parameter estimation methods. Finally, analyses of Amazon hydrological processes demonstrate that surface waters govern most of the Amazon TWS changes (56%), followed by soil water (27%) and ground water (8%). Moreover, floodplains play a major role in stream flow routing, although backwater effects are also important to delay and attenuate flood waves. Citation: Paiva, R. C. D., D. C. Buarque, W. Collischonn, M.-P. Bonnet, F. Frappart, S. Calmant, and C. A. B. Mendes (2013), Large-scale hydrologic and hydrodynamic modeling of the Amazon River basin, Water Resour. Res., 49, 1226-1243, doi: 10.1002/wrcr.20067.
引用
收藏
页码:1226 / 1243
页数:18
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