Hydrological model and integrated GIS techniques for simulation and analysis of the long-term water balance in a coastal aquifer, Spain
Metadatos
Mostrar el registro completo del ítemEditorial
Springer Nature
Materia
Water balance simulation WetSpass-M model Sensitivity analysis
Fecha
2025-07-25Referencia bibliográfica
Amen, E.M., Calvache, M.L. Hydrological model and integrated GIS techniques for simulation and analysis of the long-term water balance in a coastal aquifer, Spain. Sci Rep 15, 27148 (2025). https://doi.org/10.1038/s41598-025-07543-z
Patrocinador
Consejería de Universidad, Investigación e Innovación / Gobierno de España / Unión Europea – NextGenerationEU (PCM_00018); MICIU/AEI/10.13039/501100011033 - ERDF/EU (PID2022-137711OB-I00); MICIU/AEI/10.13039/501100011033 / EU co-financing (PCI2024-153503)Resumen
Understanding the water balance of a region as accurately as possible is essential for the optimal
and sustainable management of water resources. In this study, a hydrological model, WetSpass-M,
was used to simulate the spatial and temporal distribution of water balance components such as
the groundwater recharge, surface runoff, and actual evapotranspiration in the Motril-Salobreña
coastal aquifer (south of Spain) for the period 1980–2020. To estimate the water balance components,
data on the land use/cover, topography, slope, soil texture, irrigation allocation, and groundwater
depth were combined with meteorological data (precipitation, temperature, wind speed, and
evapotranspiration). The sensitivity analysis findings showed that the model results were affected by
the global and local parameters, specifically intensity coefficient, land and soil factors. In addition,
an agreement was observed between the simulated recharge values and those calculated using the
WTF method, with a correlation coefficient (R2) of approximately 86%, a mean error (ME) of 1.1 mm/
month, and a mean absolute error (MAE) of 2.5 mm/month. The model simulation results for water
balance components in the study area showed that of the total amount of water which enters into the
system (863 mm/year), only 19% reaches the aquifer as recharge, which represents an annual average
of approximately 164 mm. Of the remainder, 28% is surface runoff, and 53% is lost through actual
evapotranspiration. Therefore, approximately 7.2 Mm3 of water per year is recharged into the MotrilSalobreña coastal aquifer. The integration of the WetSpass model with GIS has shown its effectiveness
as a powerful approach for assessing water balance components. The model findings have also allowed
implementation of a regional groundwater model for the study area, which can be used to simulate
different aquifer management scenarios. Finally, the present study provides baseline information for
policymakers and stakeholders involved in the management and development of water resources in
the study area.





