A review is provided of the current and emerging methods for modelling catchment-scale
recharge and evapotranspiration (ET) in shallow groundwater systems. With increasing …

Simulation of large basins (over 1000 km2) can have a significant impact on the planning of
large-scale water resources management. However, due to the increasing volume of …

Distributed hydrological models have the potential to provide improved streamflow forecasts
along the entire channel network, while also simulating the spatial dynamics of …

Estimating the impacts of climate change on groundwater represents one of the most difficult
challenges faced by water resources specialists. One difficulty is that simplifying the …

One of key inputs to hydrological modeling is the potential evapotranspiration, either from
the interception (PET0) or from the soil water of root zone (PET). The Shuttleworth–Wallace …

Tropical mountain regions are characterized by strong spatial climate gradients which
together with the limited amount of data and knowledge of the underlying processes hinder …

Hawaii streams are short and steep, often producing dangerous flash floods as a result of
rainfall events that can be short but intense. The streamflow can change by a factor of 60 in …

Existing models and methods report crop coefficient (K c) as a function of time but do not
consider the variations due to surface conditions, wetting methods, meteorological …

A fully distributed, physically-based hydrologic modeling system, MIKE SHE, was used in
this study to investigate whole-watershed hydrologic response to land use changes within …

This paper attempts to assess the impact of improved estimates of areal potential
evapotranspiration (PE) on the results of two rainfall–runoff models. A network of 42 PE …