EGU22-7966, updated on 01 Apr 2022
https://doi.org/10.5194/egusphere-egu22-7966
EGU General Assembly 2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.

Identification of large-scale aquifer behavior across three decades of groundwater storage change in the western Mediterranean region

Rafael Chavez Garcia Silva1, Robert Reinecke2, Emmanouil Varouchakis3, Jaime Gómez-Hernández4, Michael Rode1, and Seifeddine Jomaa1
Rafael Chavez Garcia Silva et al.
  • 1Department of Aquatic Ecosystem Analysis and Management, Helmholtz Centre for Environmental Research‐UFZ, Magdeburg, Germany
  • 2Institute of Environmental Science and Geography, University Potsdam, Potsdam, Germany
  • 3Technical University of Crete, School of Mineral Resources Engineering, Chania, Greece
  • 4Institute of Water and Environmental Engineering, Universitat Politècnica de València, Valencia, Spain

The Mediterranean region is undergoing increasing climatic and anthropogenic pressures that challenge water security. Groundwater is a strategic resource for agriculture and water supply in the region, buffering climate change impacts. While previous studies have focused on specific aquifers' water budgets and trends at plot scales, regional dynamics remain unclear. One of the challenges for assessment is the uneven distribution of access to groundwater level monitoring data, as it's not centralized and publicly accessible in most Mediterranean countries. Here we present results that focused on analyzing the groundwater level trends in the countries with the most available groundwater level information: France, Portugal, and Spain. This study contributes to our understanding of groundwater dynamics under varying drivers and groundwater-depletion mitigation options.

As a system with 'memory,' analyzing decades of time series is essential to understand the changes, vulnerability, and resilience. For 1985-1994, 1995-2004, and 2005-2014, a trend analysis was performed on the groundwater levels for piezometers (n=844) covering these periods with considerable completeness. We identified clusters of similar groundwater level developments and categorized them into nine aquifer archetypes, for example: stable water table depth, continued depletion, groundwater level recovery, and local gaining or depleting water levels occurring in each of the three decades. Furthermore, the influence of climate and geological variables on these temporal evolutions were analyzed. Overall, about a third of the studied piezometers showed trends in at least one of the periods. Increasing depths were observed more abundantly in the first period (1985-1994), while decreasing depths were more abundant in the last period.

This work was developed in the scope of the InTheMED project. InTheMED is part of the PRIMA programme supported by the European Union's Horizon 2020 research and innovation programme under grant agreement No 1923.

How to cite: Chavez Garcia Silva, R., Reinecke, R., Varouchakis, E., Gómez-Hernández, J., Rode, M., and Jomaa, S.: Identification of large-scale aquifer behavior across three decades of groundwater storage change in the western Mediterranean region, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-7966, https://doi.org/10.5194/egusphere-egu22-7966, 2022.

Comments on the display material

to access the discussion