Modelling the potential of land use change to mitigate the impacts of climate change on future drought in the Western Cape, South Africa

被引:0
|
作者
Naik, Myra [1 ]
Abiodun, Babatunde J. [1 ,2 ]
机构
[1] Univ Cape Town, Dept Environm & Geog Sci, Climate Syst Anal Grp, Cape Town, South Africa
[2] Univ Cape Town, Nansen Tutu Ctr Marine Environm Res, Dept Oceanog, Cape Town, South Africa
关键词
EARTH SYSTEM MODEL; WATER-RESOURCES; RIVER-BASIN; PART; SWAT; CATCHMENT; CALIBRATION; YIELD; FLOW; SOIL;
D O I
10.1007/s00704-024-04995-7
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Several studies have shown that climate change may enhance the severity of droughts over the Western Cape (South Africa) in the future, but there is a dearth of information on how to reduce the impacts of climate change on water yields. This study investigates the extent to which land-use changes can reduce the projected impacts of climate change on hydrological droughts in the Western Cape catchments. For the study, the Soil Water Assessment Tool (SWAT +) model was calibrated and evaluated over several river catchments, and the climate simulation dataset from the COordinated Regional Downscaling EXperiment (CORDEX) was bias-corrected. Using the bias-corrected climate data as a forcing, the SWAT + was used to project the impacts of future climate change on water yield in the catchments and to quantify the sensitivity of the projection to four feasible land-use change scenarios in the catchments. The land-use scenarios are the spread of forest (FOMI), the restoration of shrubland (SHRB), the expansion of cropland (CRDY), and the restoration of grassland (GRSL).The model evaluation shows a good agreement between the simulated and observed monthly streamflows at four stations, and the bias correction of the CORDEX dataset improved the hydrological simulations. The climate change projection features an increase in temperature and potential evaporation, but a decrease in precipitation and all the hydrological variables. The drying occurs across the Western Cape, with the magnitude increasing with higher global warming levels (GWLs). The land-use changes alter these climate change impacts through changes in the hydrological water balance. FOMI increases streamflow and decreases runoff, while SHRB decreases streamflow and runoff. The influence of CRDY and GRSL are more complex. However, all the impacts of land-use changes are negligible compared to the impacts of climate change. Hence, land-use changes in the Western Cape may not be the most efficient strategies for mitigating the impacts of climate change on hydrological droughts over the region. The results of the study have application towards improving water security in the Western Cape river catchments.
引用
收藏
页码:6371 / 6392
页数:22
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