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For validating the models, area under receiver operating characteristics (ROC) curve was calculated.
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At a depth of −1500 m asl (Fig. 6b), modelled temperatures range between 10 and 90 °C, though most parts of the model area are not warmer than 50 °C.
The practical solution is applied to the model area of the Trkmanka catchment area.
A special landscape-ecological map has been compiled for the model area.
Examples are presented of changes affecting the structure of the landscape, the threat of erosion, elimination of flood conditions and the quality of life in the model area.
The model area is marked with a red square.
The PML method uses an absorbing region surrounding the model area.
An approximate 2500 by 2500 m grid has been applied across the Model Area (Fig. 5).
Given the depth of groundwater is generally shallow in the model area, the evapotranspiration (ET) is considered significant.
Within the model area, the uplifted crystalline crust of the Landshut-Neuöttinger High (LNH) can be seen.
Therefore, use of the PML absorbing boundary condition alternative to extending the model area greatly reduces computational costs.
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