Abstract Groundwater 18O/16O, 2H/1H, 13C/12C, 3H, and 14C data can help quantify
molecular movements and chemical reactions governing groundwater recharge, quality …

Abstract The Prediction in Ungauged Basins (PUB) initiative of the International Association
of Hydrological Sciences (IAHS), launched in 2003 and concluded by the PUB Symposium …

The diversity in hydrologic models has historically led to great controversy on the correct
approach to process-based hydrologic modeling, with debates centered on the adequacy of …

For effective catchment management and intervention in hydrological systems a process-
based understanding of hydrological connectivity is required so that: i) conceptual rather …

Baseflow is the portion of streamflow that is sustained between precipitation events, fed to
stream channels by delayed (usually subsurface) pathways. Understanding baseflow …

Groundwater interactions with mountain streams are often simplified in model projections,
potentially leading to inaccurate estimates of streamflow response to climate change. Here …

Headwater catchments are the fundamental units that connect the land to the ocean.
Hydrological flow and biogeochemical processes are intricately coupled, yet their respective …

The role of fluid residence time and catchment length scales in controlling the chemical
composition of rivers is evaluated by comparing numerical simulations and scaling …

We examined the storage dynamics and isotopic composition of soil water over 12 months in
three hydropedological units in order to understand runoff generation in a montane …

How does climate control river chemistry? Existing literature has examined extensively the
response of river chemistry to short‐term weather conditions from event to seasonal scales …