2014
DOI: 10.1016/j.catena.2014.04.005
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Modeling hydrological variability of fresh water resources in the Rio Cobre watershed, Jamaica

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Cited by 38 publications
(12 citation statements)
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“…NSE values can differ from negative values up to less than one [63]. Generally, the calibration and validation values of the SWAT model are considered to be acceptable or satisfactory performances when NSE is within the range of 0.5 and 0.65, 0.65-0.75 is considered satisfactory, while 0.75-1.00 indicate a very good performance [64][65][66]. Table 3 presents the performance ratings for NSE, as suggested by .…”
Section: Performance Assessmentmentioning
confidence: 99%
“…NSE values can differ from negative values up to less than one [63]. Generally, the calibration and validation values of the SWAT model are considered to be acceptable or satisfactory performances when NSE is within the range of 0.5 and 0.65, 0.65-0.75 is considered satisfactory, while 0.75-1.00 indicate a very good performance [64][65][66]. Table 3 presents the performance ratings for NSE, as suggested by .…”
Section: Performance Assessmentmentioning
confidence: 99%
“…Many researchers in different parts of the world have studied the impacts of climate variability and change on shifts in hydrological regimes and water resources (e.g., [25][26][27][28]). These studies assessed the current and future water resources availability and rainfall variability across the globe to support appropriate water resources planning and management.…”
Section: Introductionmentioning
confidence: 99%
“…The SWAT model is widely used in the simulation of the quality and quantity of surface and groundwater, in estimating the environmental impacts of different land use/land management practices and climate change, in calculating loads from pollutants, in evaluating best management practices, and in the simulation of various hydrological processes (runoff, infiltration, evapotranspiration, lateral flow, tile drainage, return flow, sediment etc) [15]. SWAT employs two different methods, the soil conservation services-curve number (SCS-CN) and the Green Ampt-MeinLarsen, for streamflow estimation [16][17][18][19]. Concurrent use of a digital elevation model (DEM), land use/land cover (LULC), and soil map alongside meteorological inputs also enables spatial analysis of the outputs produced by the model.…”
mentioning
confidence: 99%