Abstract Karst regions represent 7–12% of the Earth's continental area, and about one
quarter of the global population is completely or partially dependent on drinking water from …

Understanding past climatic changes allows us to better understand how our planet will
evolve in the future. One important source of information on paleoclimate is the analysis of …

Karst aquifers are important for freshwater supply, but difficult to manage, due to highly
variable water levels and spring discharge rates. Conduits are crucial for groundwater flow …

Karst aquifers are globally prized freshwater sources, posing a significant preservation
challenge. These aquifers typically exhibit dual or even triple porosities, encompassing …

Many hydrological systems exhibit complex subsurface flow and storage behavior. Runoff
observations often only provide insufficient information for unique process identification …

Groundwater flow in a well-developed karst aquifer dominantly occurs through bedding
planes, fractures, conduits, and caves created by and/or enlarged by dissolution …

Various multivariate statistical techniques (MST) can provide valuable insights into water
quality variability. Despite numerous studies in which these methods have been used, their …

More than 25% of the world's population either lives on or obtains its water from karst
aquifers, which makes the understanding of these systems essential for water resources …

Physics-based distributed models for simulating flow in karst systems are generally based
on the discrete–continuum approach in which the flow in the three-dimensional fractured …

Karst aquifers differ from unconsolidated granular aquifers with respect to their groundwater
flow behavior because of the dual-permeability characteristics (discrete conduit network …