2005
DOI: 10.1007/s10666-004-4266-0
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Effects of climate and landcover change on stream discharge in the Ozark Highlands, USA

Abstract: Stream discharge of a watershed is affected and altered by climate and landcover changes. These effects vary depending on the magnitude and interaction of the changes, and need to be understood so that local water resource availability can be evaluated and socioeconomic development within a watershed be pursued and managed in a way sustainable with the local water resources. In this study, the landcover and climate change effects on stream discharge from the Jacks Fork River basin in the Ozark Highlands of the… Show more

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Cited by 38 publications
(29 citation statements)
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“…First stream flow was simulated by using 1973 land use land cover data and 1973-1982 climate data which was considered as the base line for change study. Secondly, the flow was simulated by 2013 land use land cover data and 1973-1982 climate data [16].…”
Section: Swat Model Efficiencymentioning
confidence: 99%
“…First stream flow was simulated by using 1973 land use land cover data and 1973-1982 climate data which was considered as the base line for change study. Secondly, the flow was simulated by 2013 land use land cover data and 1973-1982 climate data [16].…”
Section: Swat Model Efficiencymentioning
confidence: 99%
“…For example, the conversions of rangeland to agriculture were pronounced in the south than in the north. The changes in land uses are reflected in surface runoff responses due to the changes that are observed in canopy structure, surface runoff curve number and surface roughness whose eventual repercussion is on sediment yield [43,63,64]. The maximum sediment yield at the sub-basinal scale occurred in sub-basin 2 for all the years under review (i.e., 2000, 2007and 2013).…”
Section: Calibration and Validationmentioning
confidence: 99%
“…Reforestation resulted in a decrease in mean annual surface water (26Ð7 mm) and streamflow (15Ð8 mm) and an increase in mean annual evapotranspiration (15Ð9 mm) and baseflow (12Ð9 mm) in Kejie watershed. Reforestation may result in a decrease in annual discharge (Guo et al, 2008;Hu et al, 2004). …”
Section: Differentiated Impact Of Land-cover/climate Changes On Hydromentioning
confidence: 99%