Discharge at the main measuring weir (Station 551) at LTER Zöbelboden as calculated based on the gauging station’s rating curve and 15 min water level sensor data. When using the data, please take into account, that this is a karst area with uncertain catchment boundaries. The runoff at the main measuring weir does therefore not represent the true total runoff of the catchment. The best estimate of the catchment area representing the main measuring weir is 576000 m². For more details see Hartmann, A.; Kralik, M.; Humer, F.; Lange, J.; Weiler, M. Identification of a karst system’s intrinsic hydrodynamic parameters: upscaling from single springs to the whole aquifer. Environmental Earth Sciences 2011, 1–13, doi:10.1007/s12665-011-1033-9.

This repository contains the datasets collected by a monitoring network of 4 discharge gauging stations, 7 rain-gauges, together with observations of air and water temperature, relative humidity and conductivity. In four profiles, soil water content and temperature are recorded in different depths. In 2019, additionally a program to collect isotopic data in precipitation and discharge was started. On one site, also Nitrate, TOC and turbidity are monitored. All data collected since 2015, including in total 56 high resolution time series data (10 min sampling interval), are provided to the scientific community. Updates are planned annually, as soon as the raw data of the previous year are checked for plausibility.