Estimating of the impact of land use changes using the conceptual hydrological model THESEUS––a case study

• Published in: Physics and chemistry of the earth. Parts A/B/C Vol. 27; no. 9; pp. 631 - 640
• Main Author: Wegehenkel, Martin
• Format: Journal Article
• Language: English
• Published: Elsevier Ltd 01-01-2002
• Subjects: Discharge; Germany; Hydrological modelling; Land use effects; Water balance; Germany, Brandenburg; Hydrological modelling; Water balance; Land use effects; Discharge
• ISSN: 1474-7065; 1873-5193
• DOI: 10.1016/S1474-7065(02)00047-5

As a result of a new agricultural funding policy established in 1992 by the European Community, it was assumed that up to 15–20% of arable land would have been set aside in the next years in the new federal states of north-eastern Germany, for example, Brandenburg.
As one potential land use option, afforestation of these set aside areas was discussed to obtain deciduous forests. Since the mean annual precipitation in north-eastern Germany, Brandenburg is relatively low (480–530 mm
y
−1), an increase in interception and evapotranspiration loss by forests compared to arable land would lead to a reduction in ground water recharge. Experimental evidence to determine effects of such land use changes are rarely available. Therefore, there is a need for indirect methods to estimate the impact of afforestation on the water balance of catchments.
In this paper, a conceptual hydrological model was verified and calibrated in two steps using data from the Stobber-catchment located in Brandenburg. In the first step, model outputs like daily evapotranspiration rates and soil water contents were verified on the basis of experimental data sets from two test locations. One test site with the land use arable land was located within the Stobber-catchment. The other test site with pine forest was located near by the catchment. In the second step, the model was used to estimate the impact of afforestation on catchment water balance and discharge. For that purpose, the model was calibrated against daily discharge measurements for the period 1995–1997. For a simple afforestation scenario, it was assumed that the area of forest increases from 34% up to 80% of the catchment area. The impact of this change in forest cover proportion was analyzed using the calibrated model. In case of increasing the proportion of forest cover in the catchment due to the scenario afforestation, the model predicts a reduction in discharge and an increase in evapotranspiration.