Application of the SWAT model to assess climate and land use/cover change impacts on water balance components of the Kabul River Basin, Afghanistan

Water resources Representative Concentration Pathways Climate Change and Variability Research Precipitation Oceanography Environmental technology. Sanitary engineering 01 natural sciences Climate change GE1-350 TD1-1066 Water Science and Technology Climatology Global and Planetary Change Evapotranspiration Geography Ecology kabul river basin Soil and Water Assessment Tool Hydrology (agriculture) Geology 6. Clean water Surface Water Mapping climate change Hydrological Modeling and Water Resource Management Physical Sciences SWAT model water balance components land use change Cartography Land cover Hydrological Modeling Drainage basin Streamflow Climate model Environmental science Global Flood Risk Assessment and Management Meteorology swat model Machine learning Water balance Biology Land use, land-use change and forestry 0105 earth and related environmental sciences Baseline (sea) FOS: Earth and related environmental sciences 15. Life on land Watershed Simulation Watershed Computer science Environmental sciences Geotechnical engineering 13. Climate action FOS: Biological sciences Environmental Science Land use Flood Inundation Modeling Climate Modeling
DOI: 10.2166/wcc.2022.261 Publication Date: 2022-11-08T12:15:33Z
ABSTRACT
Abstract Hydrological models play a key role in simulating and assessing climate and land use/cover (LULC) change impacts on hydrology in a watershed. In this study, the impact of climate and LULC change was investigated using the Soil and Water Assessment Tool (SWAT) model. The simulated and observed streamflow showed a good agreement. Both Nash–Sutcliffe Efficiency (NSE) and coefficient of determination (R2) were found to be greater than 0.7 during the calibration (1985–2002) and validation (2003–2012) period. The water balance components were simulated with inputs from downscaled Global Climate Models (GCMs) data (i.e., future scenario (2030–2100) relative to a baseline period (1974–2004)) under RCP4.5 and RCP8.5, and hypothetical generated LULC change scenarios. All GCMs projected an increase in temperature over the Kabul River Basin (KRB), whereas there was a lack of agreement on projected precipitation among GCMs under both emission and future scenarios. Water yield (WYLD) and evapotranspiration (ET) were projected to decrease in the 21st century. Average annual WYLD was projected to increase under the agriculture-dominant scenario, whereas it decreased under forest and grassland-dominant scenarios. These results are valuable for relevant agencies and stakeholders to adopt measures to counter the negative impacts of climate and LULC change on water resources.
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