Journal
HYDROLOGICAL SCIENCES JOURNAL-JOURNAL DES SCIENCES HYDROLOGIQUES
Volume 55, Issue 4, Pages 636-648Publisher
TAYLOR & FRANCIS LTD
DOI: 10.1080/02626661003780409
Keywords
sediment yield; watershed connectivity; catchment scale; semi-arid; WASA-SED model
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Funding
- CAPES (Coordenacao de Aperfeicoamento do Pessoal de Nivel Superior, Ministry of Education, Brazil)
- DAAD (Deutscher Akademischer Austausch Dienst, Germany)
- German Research Foundation (DFG)
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Rainfall-runoff induced soil erosion causes important environmental degradation by reducing soil fertility and impacting on water availability as a consequence of sediment deposition in surface reservoirs used for water supply, particularly in semi-arid areas. However, erosion models developed on experimental plots cannot be directly applied to estimate sediment yield at the catchment scale, since sediment redistribution is also controlled by the transport conditions along the landscape. In particular, representation of landscape connectivity relating to sediment transfer from upslope areas to the river network is required. In this study, the WASA-SED model is used to assess the spatial and temporal patterns of water and sediment connectivity for a semi-arid meso-scale catchment (933 km(2)) in Brazil. It is shown how spatial and temporal patterns of sediment connectivity within the catchment change as a function of landscape and event characteristics. This explains the nonlinear catchment response in terms of sediment yield at the outlet.
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