Catchments, generally understood as the drainage areas of low‐order streams, are often
regarded as closed hydrologic entities; that is, precipitation (P) minus evapotranspiration …

One of the main challenges in water management is to determine how the current water use
can condition its availability to future generations and hence its sustainability. This study …

Measurement and monitoring of the pollution in continental waters is one of the main
challenges in water resources management as pollution is the principal cause of …

Currently, climate change is a major concern around the world, especially because of the
uncertainty associated with its possible consequences for society. Among them, fluvial …

Stream gauging stations provide critical streamflow measurements for hydrological
applications; however, they may not accurately capture total catchment discharge due to …

For a better understanding of the spatial variability of the hydrological response of
catchments to flood events, the hydrological indicators obtained from annual water balances …

Karst hydrological models are widely used for simulating groundwater dynamics at the
aquifer scale. However, modeling streamflow of a topographic catchment that is partially …

Inter-basin groundwater flow (IGF), defined as groundwater flows across the topographic
divides, occurs in nature as a common phenomenon, and seriously affect water balance and …

Aquifer systems, because of the presence of frequently complex geological structures, may
extend beyond watersheds limits. Interbasin groundwater flow is often identified among …

In most water balance studies, basins are considered closed systems; however, interbasin
groundwater flow (IGF), which is an unaccounted hydrological component in most studies …