Assessing the Impact of Climate Change on Water Scarcity in the Tormes Catchment, Spain: A Human-Water System Modeling Approach
- 1Department of Economics and Economic History, Universidad de Salamanca, Spain (osama003@usal.es)
- 2Department of Economics and Economic History, Universidad de Salamanca, Spain (dionisio.perez@usal.es)
- 3Department of Economics and Economic History, Universidad de Salamanca, Spain (hector.gonzalez.lopez@usal.es)
Climate change presents a pressing challenge to global water availability resulting in increased variability in precipitation and increased temperatures, imposing more stress on existing water resources and the economic activities that depend on them. The Tormes catchment, located in a semi-arid region, is facing increasingly severe water shortages, which may be further aggravated under climate change. This catchment is extensively employed for agricultural purposes, and a potential reduction in the availability of water for irrigation emerges as a significant concern.
This study evaluates the impact of climate change on water availability, and the responses implemented by irrigators to adapt to growing scarcity, in the Tormes catchment. To this end, we develop a human-water system model that couples the Soil and Water Assessment Tool (SWAT) model and a Positive Multi-Attribute Utility Programming (PMAUP) model using a dynamic and modular approach. The coupled model runs the water (SWAT) and human (PMAUP) system models iteratively and over time using inputs from six different bias-corrected Global Climate Models(GCMs) under CMIP6 scenarios, as follows: i) CMIP6 climate change scenario simulations are fed to the SWAT model to estimate relevant hydrological data including water availability in March (beginning of the irrigation campaign); ii) information on water availability is fed to the PMAUP model to simulate the adaptive responses of irrigators in terms of water and land allocation; iii) land and water use choices by irrigators are fed into the SWAT model, which reproduces the consequences of human decisions on the water system; iv) when the hydrological year is over, a new iteration starts where CMIP6 climate change scenario simulations for the following year are fed into the SWAT model and the process is repeated again. The non-linearity and modular approach in both the hydrological and economic models imply complex and interconnected interactions within these systems, with behaviors that may or may not follow linear patterns.
Six bias-corrected GCMs under CMIP6 scenarios were employed for the climate change scenario simulations. The dataset covered precipitation, maximum and minimum temperatures for the historical period (1981–2010) and projections for SSP245 and SSP585. Future data was analyzed for three periods: 2020–2039, 2040–2059, and 2060–2100. A multi-model ensemble approach was applied, averaging outputs from the six models. Precipitation and temperature data were integrated into the SWAT model.
The hydrological analysis revealed a downward trend in projected precipitation, with reductions of 0.7% (2020s), 0.3% (2040s), and up to 5.3% (2060s) under SSP245. SSP585 showed declines of 6.4% (2020s), 6.6% (2040s), and 16.1% (2060s). Maximum and minimum temperatures exhibited an upward trend under both scenarios. Simulated mean annual runoff under SSP245 experienced a drastic reduction of 48.1% in the 2020s, followed by 43.8% (2040s) and 53% (2060s). Similarly, under SSP585, mean annual runoff decreased by 47.2% over the entire projection period. While the hydrological analysis reveals concerning trends in precipitation, temperature, and mean annual runoff under different scenarios, the economic results, reflecting the effects of these hydrological changes on human activities, are still being investigated and are not yet finalized.
How to cite: Hassan, O. G. B., Pérez-Blanco, C. D., and González-López, H.: Assessing the Impact of Climate Change on Water Scarcity in the Tormes Catchment, Spain: A Human-Water System Modeling Approach, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-4678, https://doi.org/10.5194/egusphere-egu24-4678, 2024.