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Investigation of soil water budget in the unsaturated soil zone is commonly performed for determination of the complex relationships between the different components of the water budget. A main focus of this work was on acquisition and evaluation of percolation water and soil moisture dynamics depending on the site properties (climate, soils, land use). A network consisting of 14 lysimeter and soil moisture measuring stations was established in the region of the Trier-Bitburger-Mulde (SW-Eifel, Germany). During a period of four hydrological years precipitation, infiltration, percolation water and soil moisture were collected weakly on the stations comprising the different regional characteristics of soil textures and land use patterns. The analysis of the weekly data sets enabled to point out seasonal variations of percolation water and soil water dynamics (as time-depth function). Comparison of simultaneously collected data sets of percolation water, soil moisture, and evapotranspiration shows significant fluctuations, which result from the complex relationships between the site properties. Hereby, the soil properties and in particular the secondary macropores (root channels, shrinkage- /frost cracks) have a striking influence on the variability of the water flows in the unsaturated soil zone. The results of the GIS-based regionalisation of the annual amount of percolation water prove the influence of topography (relief conditions, especially slope and aspect) on percolation and soil water dynamics in low mountain ranges.
The United States insisted that the International Criminal Court would not have jurisdiction to prosecute American nationals. It was to be a court for others, not for them. The Rome Conference insisted on upholding the principle of equal justice for all and consequently rejected American exceptionalism. The Clinton administration nevertheless signed the ICC Statute and remained involved in the post Rome proceedings of the Preparatory Commission for the International Criminal Court. However, when President Bush took office, his administration embarked on a world wide campaign to discredit the ICC. It cancelled the American signing of the ICC Statute, it enacted hostile legislation aimed at frustrating the functioning of the ICC, and it concluded agreements with approximately 50 States that place those States under an obligation not to surrender American nationals for trial in the ICC. The difference of opinion between the United States and the European Union cannot be resolved by diplomatic means since the United States administration is obligated by an American statute to discredit the ICC and to prevent it from operating according to its Statute. The European Union and its Member States will therefore have to embark on a policy of confrontation.
Considering actual climatic and land use changes the problem of available water resources or the estimation of potential flood risks gain eco-political and economical relevance. Adequate assessments, thus, require precise process-based hydrological knowledge. Spatially distributed hydrological modelling enables a both abstractive and realistic description of hydrological processes, and therefore contributes to the understanding of the hydrological system- responses. Referring to the example of the mesoscale Ruwer basin (a tributary to the Mosel river), a modified version of the distributive modelling system PRMS/MMS (Precipitation Runoff Modeling System/Modular Modeling System) is applied to calculate spatially and temporally explicit water budgets. To achieve modelling results as precise as possible, integration of detailed land use information (spatial distribution of the existing land use classes, crop- and site-specific growth patterns) is necessary. This information is derived here by analysis of multitemporal, geometrically and radiometrically pre-processed Landsat TM-data. This enables separation of different land use classes and differentiated quantification of the leaf area index (LAI). The LAI is estimated by a spectral unmixing approach using statistically optimized endmember sets, referring to the example of winter grain and grassland plots. As a result, numerical inputs (coefficients for calculating evapotranspiration, interception storages) and extracted non-numerical (classified) information can be provided for hydrological modelling. The version of PRMS applied in this study allows important land use terms to be parameterized in high temporal resolution. Using model input derived from the available satellite data, simulation results are obtained that prove to be realistic compared to gauge data and with respect to their spatial differentiation. Results differ significantly from those obtained by using parameters from literature or by experience without distinguishing specific and site-dependent growth patterns. It can be concluded that the quality of modelling results notably improves by integration and quantitative analysis of remote sensing data; thus, these methods are a significant contribution to physically-based hydrological modelling.
Software and interactive systems that adapt their behavior to the user are often referred to as Adaptive Systems. These systems infer the user's goals, knowledge or preferences by observing the user's actions. A synposis of 43 published studies demonstrated that only few of the existing systems are evaluated empirically. Most studies failed to show an advantage of the user model. A new framework is proposed that categorizes existing studies and defines an evaluation procedure which is able to uncover failures and maladaptations in the user model. It consists of four layers: evaluation of input data, evaluation of inference, evaluation of adaptation decision and evaluation of total interaction. Exemplary, the framework has been applied to the HTML-Tutor, an online-course that adapts to the learners' knowledge. Several empirical studies are described that test the accuracy of the user models, and explore the effects of adaptation to knowledge respectively prior knowledge. Generalization issues of the approach are discussed.