Seawater intrusion in coastal aquifers is a worldwide problem exacerbated by aquifer overexploitation and climate changes. To limit the deterioration of water quality caused by saline intrusion, research studies are needed to identify and assess the performance of possible countermeasures, e.g., underground barriers. Within this context, numerical models are fundamental to fully understand the process and for evaluating the effectiveness of the proposed solutions to contain the saltwater wedge; on the other hand, they are typically affected by uncertainty on hydrogeological parameters, as well as initial and boundary conditions. Data assimilation methods such as the ensemble Kalman filter (EnKF) represent promising tools that can reduce suc...
Electrical resistivity tomography (ERT) can be used to constrain seawater intrusion models because o...
Electrical resistivity tomography (ERT) can be used to constrain seawater intrusion models because o...
Estimating the spatial variability of hydraulic conductivity K in natural aquifers is important for ...
Evolutionary optimization algorithms are known as reliable optimization methods, but they are typica...
Hydraulic properties of natural aquifers, such as porosity, hydraulic conductivity, and storativity,...
The ensemble Kalman filter (EnKF) is a powerful tool for assimilating data in earth system models. T...
The ensemble Kalman filter (EnKF) is a powerful tool for assimilating data in earth system models. T...
The ensemble Kalman filter (EnKF) is a powerful tool for assimilating data in earth system models. T...
In this study the ensemble Kalman filter (EnKF) is implemented in a detailed catchment-scale hydrolo...
The ensemble Kalman filter (EnKF) is a powerful tool for assimilating data in earth system models. T...
Borehole ERT monitoring of saline tracer tests allows to collect time-lapse geophysical data as chan...
Borehole ERT monitoring of saline tracer tests allows to collect time-lapse geophysical data as chan...
Recent advances in geophysical methods have been increasingly exploited as inverse modeling tools in...
Management of groundwater resources has become a source of heated discussion in coastal hydrogeology...
Electrical resistivity tomography (ERT) can be used to constrain seawater intrusion models because o...
Electrical resistivity tomography (ERT) can be used to constrain seawater intrusion models because o...
Electrical resistivity tomography (ERT) can be used to constrain seawater intrusion models because o...
Estimating the spatial variability of hydraulic conductivity K in natural aquifers is important for ...
Evolutionary optimization algorithms are known as reliable optimization methods, but they are typica...
Hydraulic properties of natural aquifers, such as porosity, hydraulic conductivity, and storativity,...
The ensemble Kalman filter (EnKF) is a powerful tool for assimilating data in earth system models. T...
The ensemble Kalman filter (EnKF) is a powerful tool for assimilating data in earth system models. T...
The ensemble Kalman filter (EnKF) is a powerful tool for assimilating data in earth system models. T...
In this study the ensemble Kalman filter (EnKF) is implemented in a detailed catchment-scale hydrolo...
The ensemble Kalman filter (EnKF) is a powerful tool for assimilating data in earth system models. T...
Borehole ERT monitoring of saline tracer tests allows to collect time-lapse geophysical data as chan...
Borehole ERT monitoring of saline tracer tests allows to collect time-lapse geophysical data as chan...
Recent advances in geophysical methods have been increasingly exploited as inverse modeling tools in...
Management of groundwater resources has become a source of heated discussion in coastal hydrogeology...
Electrical resistivity tomography (ERT) can be used to constrain seawater intrusion models because o...
Electrical resistivity tomography (ERT) can be used to constrain seawater intrusion models because o...
Electrical resistivity tomography (ERT) can be used to constrain seawater intrusion models because o...
Estimating the spatial variability of hydraulic conductivity K in natural aquifers is important for ...