Process-based hydrological models have a long history dating back to the 1960s. Criticized
by some as over-parameterized, overly complex, and difficult to use, a more nuanced view is …

Integrated, process‐based numerical models in hydrology are rapidly evolving, spurred by
novel theories in mathematical physics, advances in computational methods, insights from …

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Zero-order drainage basins, and their constituent hillslopes, are the fundamental
geomorphic unit comprising much of Earth's uplands. The convergent topography of these …

Hillslope‐scale rainfall‐runoff processes leading to a fast catchment response are not
explicitly included in land surface models (LSMs) for use in earth system models (ESMs) due …

Monitoring water status near the soil surface is a prerequisite for studying hydrological
processes at the soil-atmosphere boundary and an option for calibrating remotely sensed …

A seepage face is a nonlinear dynamic boundary that strongly affects pressure head
distributions, water table fluctuations, and flow patterns. Its handling in hydrological models …

Spatially integrated water transport dynamics at the hillslope scale have rarely been
observed directly, and underlying physical mechanisms of those dynamics are poorly …

Groundwater is the most abundant freshwater resource and it needs protection and
sustainable management. Therefore, knowing the groundwater level is important for many …

In arid and semiarid climate catchments, where annual evapotranspiration (ET) and rainfall
are typically comparable, modeling ET is important for proper assessment of water …