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
AUTHORS (3)
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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CITATIONS (25)
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