Inverse modelling is a key step in groundwater-related hydrological studies. Several inversion techniques were developed during the last decades, but hardly any comparison between them was presented. We compare seven modern inverse methods for groundwater flow: the Regularised Pilot Points Method (both the estimation, RPPM-CE, and the Monte Carlo (MC) simulation variants, RPPM-CS), the MC variant of the Representer Method (RM), the Sequential Self-Calibration Method (SSC), the Moment Equations Method (MEM), the Zonation Method (ZM) and a non-iterative Semi-Analytical Method (SAM). These methods are applied to a two-dimensional synthetic example, depicting steady-state groundwater flow around a pumping well. Their relative performance is ...
The use of inverse methods allow efficient model calibration. This study employs PEST to calibrate a...
[EN] Parameter identification is an essential step in constructing a groundwater model. The process ...
We derive and solve novel equations satisfied by the exact sensitivity matrix of the (ensemble) mean...
Inverse modelling is a key step in groundwater-related hydrological studies. Several inversion techn...
Inverse modelling is a key step in groundwater-related hydrological studies. Several inversion techn...
Inverse modelling is a key step in groundwater-related hydrological studies. Several inversion techn...
The basic classical inverse problem of groundwater hydrology aims at determining aquifer transmissiv...
The use of inverse methods allow efficient model calibration. This study employs PEST to calibrate a...
The use of inverse methods allow efficient model calibration. This study employs PEST to calibrate a...
The impact of various sources of uncertainty on predictions of groundwater flow is conveniently tack...
The impact of various sources of uncertainty on predictions of groundwater flow is conveniently tack...
The impact of various sources of uncertainty on predictions of groundwater flow is conveniently tack...
The impact of various sources of uncertainty on predictions of groundwater flow is conveniently tack...
The use of inverse methods allow efficient model calibration. This study employs PEST to calibrate a...
The use of inverse methods allow efficient model calibration. This study employs PEST to calibrate a...
The use of inverse methods allow efficient model calibration. This study employs PEST to calibrate a...
[EN] Parameter identification is an essential step in constructing a groundwater model. The process ...
We derive and solve novel equations satisfied by the exact sensitivity matrix of the (ensemble) mean...
Inverse modelling is a key step in groundwater-related hydrological studies. Several inversion techn...
Inverse modelling is a key step in groundwater-related hydrological studies. Several inversion techn...
Inverse modelling is a key step in groundwater-related hydrological studies. Several inversion techn...
The basic classical inverse problem of groundwater hydrology aims at determining aquifer transmissiv...
The use of inverse methods allow efficient model calibration. This study employs PEST to calibrate a...
The use of inverse methods allow efficient model calibration. This study employs PEST to calibrate a...
The impact of various sources of uncertainty on predictions of groundwater flow is conveniently tack...
The impact of various sources of uncertainty on predictions of groundwater flow is conveniently tack...
The impact of various sources of uncertainty on predictions of groundwater flow is conveniently tack...
The impact of various sources of uncertainty on predictions of groundwater flow is conveniently tack...
The use of inverse methods allow efficient model calibration. This study employs PEST to calibrate a...
The use of inverse methods allow efficient model calibration. This study employs PEST to calibrate a...
The use of inverse methods allow efficient model calibration. This study employs PEST to calibrate a...
[EN] Parameter identification is an essential step in constructing a groundwater model. The process ...
We derive and solve novel equations satisfied by the exact sensitivity matrix of the (ensemble) mean...