Mots-clés
Adaptation ; Bassin-versant ; Bilan hydrologique ; Changement climatique ; Eau douce ; Espace-temps ; Hydrologie ; Jamaïque ; Modèle ; Ressource en eau ; Rio Cobre ; Utilisation du solAdaptation ; Climatic change ; Fresh water ; Hydrology ; Jamaica ; Land use ; Model ; Space time ; Water balance ; Water resources ; WatershedAdaptación ; Agua dulce ; Aprovechamiento del suelo ; Balance hidrológico ; Cambio climático ; Cuenca hidrográfica ; Espacio-tiempo ; Hidrología ; Jamaica ; Modelo ; Recursos en aguaModeling hydrological variability of fresh water resources in the Rio Cobre watershed, Jamaica
Auteur(s) et Affiliation(s)
SETEGN, S.G.
Dept. of Environmental and Occupational Health and Global Water for Sustainability, Miami, Etats-Unis
GLOWS, Florida International Univ., Miami, Etats-Unis
MELESSE, A.M.
Dept. of Earth and Environment, Florida International Univ., Miami, Etats-Unis
HAIDUK, A.
Water Resources Authrity, Hope Gardens, Kingston, Jamaique
WEBBER, D.
Dept. of life Sciences, Univ. of the West Indies, Kingston, Jamaique
WANG, X.
Dept. of Civil and Environmental Engineering, Univ., Old Domnion, Etats-Unis
MCCLAIN, M.E.
Dept. of Water Science and Engineering, UNESCO-IHE Inst. for Water Education, Delft, Pays-Bas
Fac. of Civil Engineering and Geosciences, Univ. of Technology, Delft, Pays-Bas
Description :
The aim of this study is to characterize, model and analyze the temporal variability of hydrological processes in the Rio Cobre watershed, Jamaica using the Soil and Water Assessment Tool (SWAT). Determination of the temporal hydrological water balance and the spatial distribution of hydrological processes in the Rio Cobre watershed are discussed. The ability of a watershed model to accurately predict the hydrological processes is evaluated through parameter sensitivity analysis, model calibration and validation. Sequential Uncertainty Fitting (SUFI-2) calibration and uncertainty analysis methods were used for the set-up of the SWAT model. The model evaluation statistics for streamflow prediction show that there is a good agreement between the measured and simulated flows. The spatiotemporal distribution of hydrological processes was determined. It is highlighted that 52% of rainfall is lost by evapotranspiration and that the groundwater contributes 42% to the water yield.
Type de document :
Article de périodique
Source :
Catena (Giessen), issn : 0341-8162, 2014, vol. 120, p. 81-90, nombre de pages : 10, Références bibliographiques : 20 ref.
Date :
2014
Editeur :
Pays édition : Allemagne, Cremlingen-Destedt, Catena
Langue :
Anglais
Anglais
Droits :
Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI)
Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI)