The time that water takes to travel through the terrestrial hydrological cycle and the critical
zone is of great interest in Earth system sciences with broad implications for water quality …

Water stable isotopes (18O and 2H) are widely used as ideal tracers to track water through
the soil and to separate evaporation from transpiration. Due to the technical developments in …

In spite of trying to understand processes in the same spatial domain, the catchment
hydrology and water quality scientific communities are relatively disconnected and so are …

Protecting or restoring aquatic ecosystems in the face of growing anthropogenic pressures
requires an understanding of hydrological and biogeochemical functioning across multiple …

Understanding the influence of vegetation on water storage and flux in the upper soil is
crucial in assessing the consequences of climate and land use change. We sampled the …

Climate change is expected to alter hydrological and biogeochemical processes in high-
latitude inland waters. A critical question for understanding contemporary and future …

Observations and data from long‐term experimental watersheds are the foundation of
hydrology as a geoscience. They allow us to benchmark process understanding, observe …

Quantifying how vegetation mediates water partitioning at different spatial and temporal
scales in complex, managed catchments is fundamental for long-term sustainable land and …

We use high‐resolution tracer data from an experimental site to test theoretical approaches
that integrate catchment‐scale flow and transport processes in a unified framework centered …

Water transit time is now a standard measure in catchment hydrological and ecohydrological
research. The last comprehensive review of transit time modeling approaches was …