The interaction between surface water and groundwater constitutes a critical process to
understand the quantitative and qualitative regime of dependent hydrosystems. A multi …

Driven by the need for integrated management of groundwater (GW) and surface water
(SW), quantification of GW–SW interactions and associated contaminant transport has …

Groundwater discharge generates streamflow and influences stream thermal regimes.
However, the water quality and thermal buffering capacity of groundwater depends on the …

This review surveys the basic theories, observational methods, satellite algorithms, and land
surface models for terrestrial evapotranspiration, E (or λE, ie, latent heat flux), including a …

Humic substances (HS), a highly transformed part of non-living natural organic matter
(NOM), comprise up to 70% of the soil organic matter (SOM), 50–80% of dissolved organic …

Karst aquifers, capable of storing and transmitting large amount of water, are the main
source of drinking water in many regions worldwide. Their excessive permeability leads to …

Rivers are important ecosystems under continuous anthropogenic stresses. The hyporheic
zone is a ubiquitous, reactive interface between the main channel and its surrounding …

River‐groundwater interactions are at the core of a wide range of major contemporary
challenges, including the provision of high‐quality drinking water in sufficient quantities, the …

Scientists and practitioners agree that integrated water resource management is necessary,
with an increasing need for research at the regional scale (10 3 to 10 5 km 2). At this scale …

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