Calibration and evaluation of a semi-distributed watershed model of Sub-Saharan Africa using GRACE data

被引:55
作者
Xie, H. [1 ]
Longuevergne, L. [2 ]
Ringler, C. [1 ]
Scanlon, B. R. [3 ]
机构
[1] Int Food Policy Res Inst, Washington, DC 20006 USA
[2] Geosci Rennes Univ Rennes 1, CNRS UMR 6118, F-35042 Rennes, France
[3] Univ Texas Austin, Jackson Sch Geosci, Bur Econ Geol, Austin, TX 78713 USA
基金
比尔及梅琳达.盖茨基金会;
关键词
LAND-SURFACE MODEL; HYDROLOGIC-MODELS; GRAVITY-FIELD; SOIL-MOISTURE; RIVER; ASSIMILATION; VARIABILITY; ALGORITHM;
D O I
10.5194/hess-16-3083-2012
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Irrigation development is rapidly expanding in mostly rainfed Sub-Saharan Africa. This expansion underscores the need for a more comprehensive understanding of water resources beyond surface water. Gravity Recovery and Climate Experiment (GRACE) satellites provide valuable information on spatio-temporal variability in water storage. The objective of this study was to calibrate and evaluate a semi-distributed regional-scale hydrologic model based on the Soil and Water Assessment Tool (SWAT) code for basins in Sub-Saharan Africa using seven-year (July 2002-April 2009) 10-day GRACE data and multi-site river discharge data. The analysis was conducted in a multi-criteria framework. In spite of the uncertainty arising from the trade-off in optimising model parameters with respect to two non-commensurable criteria defined for two fluxes, SWAT was found to perform well in simulating total water storage variability in most areas of Sub-Saharan Africa, which have semi-arid and sub-humid climates, and that among various water storages represented in SWAT, water storage variations in soil, vadose zone and groundwater are dominant. The study also showed that the simulated total water storage variations tend to have less agreement with GRACE data in arid and equatorial humid regions, and model-based partitioning of total water storage variations into different water storage compartments may be highly uncertain. Thus, future work will be needed for model enhancement in these areas with inferior model fit and for uncertainty reduction in component-wise estimation of water storage variations.
引用
收藏
页码:3083 / 3099
页数:17
相关论文
共 75 条
[1]   Global Evaluation of the ISBA-TRIP Continental Hydrological System. Part I: Comparison to GRACE Terrestrial Water Storage Estimates and In Situ River Discharges [J].
Alkama, R. ;
Decharme, B. ;
Douville, H. ;
Becker, M. ;
Cazenave, A. ;
Sheffield, J. ;
Voldoire, A. ;
Tyteca, S. ;
Le Moigne, P. .
JOURNAL OF HYDROMETEOROLOGY, 2010, 11 (03) :583-600
[2]   Increasing River Flows in the Sahel? [J].
Amogu, Okechukwu ;
Descroix, Luc ;
Yero, Kadidiatou Souley ;
Le Breton, Eric ;
Mamadou, Ibrahim ;
Ali, Abdou ;
Vischel, Theo ;
Bader, Jean-Claude ;
Moussa, Ibrahim Bouzou ;
Gautier, Emmanuele ;
Boubkraoui, Stephane ;
Belleudy, Philippe .
WATER, 2010, 2 (02) :170-199
[3]  
[Anonymous], 2010, STATE FOOD INSECURIT
[4]  
[Anonymous], 2007, Water for Food, Water for Life: A Comprehensive Assessment of Water Management in Agriculture, DOI DOI 10.4324/9781849773799
[5]  
[Anonymous], 1972, HYDR NAT ENG HDB
[6]   Large area hydrologic modeling and assessment - Part 1: Model development [J].
Arnold, JG ;
Srinivasan, R ;
Muttiah, RS ;
Williams, JR .
JOURNAL OF THE AMERICAN WATER RESOURCES ASSOCIATION, 1998, 34 (01) :73-89
[7]   Recent hydrological behavior of the East African great lakes region inferred from GRACE, satellite altimetry and rainfall observations [J].
Becker, Melanie ;
LLovel, William ;
Cazenave, Anny ;
Guentner, Andreas ;
Cretaux, Jean-Francois .
COMPTES RENDUS GEOSCIENCE, 2010, 342 (03) :223-233
[8]  
Bettadpur S., 2007, LEVEL 2 GRAVITY FIEL
[9]   THE FUTURE OF DISTRIBUTED MODELS - MODEL CALIBRATION AND UNCERTAINTY PREDICTION [J].
BEVEN, K ;
BINLEY, A .
HYDROLOGICAL PROCESSES, 1992, 6 (03) :279-298
[10]   CNES/GRGS 10-day gravity field models (release 2) and their evaluation [J].
Bruinsma, Sean ;
Lemoine, Jean-Michel ;
Biancale, Richard ;
Vales, Nicole .
ADVANCES IN SPACE RESEARCH, 2010, 45 (04) :587-601