Titlebook: EuroKarst 2022, Málaga; Advances in the Hydr Bartolomé Andreo,Juan Antonio Barberá,Matías Mudar Conference proceedings 2023 The Editor(s) (

小步舞

Deriving Major Ion Concentrations at High Resolution from Continuous Electrical Conductivity Measureus complexes are obtained from speciation calculations. The method is tested in two karstic watersheds with different types of bedrock and temporal resolution of the available hydrochemical datasets, i.e. the Kerschbaum dolostone system in Austria and the Baget limestone system in France. The result

LOPE

Hydrogeological Characterization and Modeling at Two Test Sites of the Apulian Karst (Southern Italy understand the hydrodynamics of karst systems. The final aim of this research, still ongoing, is to integrate and use surface and subsurface geological data in order to obtain more realistic model outputs.

RLS898

Prediction of Future Interactions Between Karst and River Regarding to Climate Change Based on IPCC arstic catchment of the Gorges and the Cèze river and then to predict their evolution regarding to climate change scenarios. The model has been developed using KarstMod software, which consists in an adjustable modelling platform. Firstly, the model has been calibrated on one hydrological cycle and

刚开始

On the Choice of a Performance Metric for Model Calibration Scheme Using Discharge-Age Information young water age, we not only satisfy the minimization of model simulation bias but also bring the process-based discharge-age information content into the model parametrization. To test our hypothesis, we applied our approach to one of the karstic water sources in Austria. Our finding indicates tha

WITH

生气地

Conference proceedings 2023ook is a resource for scientists around the world to compare problems, results, and solutions. Likewise, the examples included are used in policy decision making in karst regions. Finally, the contributions are used as a tool for university teaching.

昆虫

Acumen

,Das Ausreiben und Versenken der Nietlöcher,g floods, while springs and swallow holes discharges measurements are impossible, the extension of the flooded areas has been mapped. The obtained flooded surface together with high resolution DTM coverage allows to calculate the volume of surface water. Consequently, the hydrologic balance can be e

玉米

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