Karst water resources are estimated to provide drinking water to 10%-25% of the world's population (Ford & Williams, 2007; Stevanović, 2019). In some countries and regions, for example, Austria and Slovenia, karst water resources account for approximately half of the total water supply (Hartmann, Goldscheider, et al., 2014; Stevanović, 2019). Chemical weathering of carbonate rock results in a strong subsurface heterogeneity in karstic areas, which leads to groundwater recharge and storage behavior substantially different from the nonkarstic regions (Bakalowicz, 2005; Hartmann & Baker, 2017). Climate projections suggest strong changes of temperature and precipitation in almost all karstic regions in the world (Christensen et al., 2007). Climate change will affect hydrological dynamics and water availability in karstic regions by an unknown extent. New approaches to understanding the impact of climate change on karstic regions are therefore of great importance. Recent achievements in karst research include the creation of a karst spring discharge database to promote data availability for karstic regions (Olarinoye et al., 2020), relating soil moisture networks to karst groundwater storage and flow (Berthelin et al., 2020), using tracer experiments to detect fast and slow pathways and the connectivity of conduit systems (