In seasonally dry environments, critical zone drainage provides base flow that sustains river
ecosystems. The extent of wetted channels and magnitude of base flow throughout the …

Alluvial aquifers in mountainous regions cover typically a limited area. Their contribution to
catchment storage and outflow is rarely isolated; alluvial groundwater discharge under …

Streamflow monitoring in the Colorado River Basin (CRB) is essential to ensure diverse
needs are met, especially during periods of drought or low flow. Existing stream gage …

Limited geo-hydro-meteorological data availability in most of the subsurface water
catchments world-wide has constrained the effective surface and subsurface water …

Traditional Boussinesq or kinematic simulations of interflow (ie, lateral subsurface flow)
assume no leakage through the impeding layer and require a no‐flow boundary condition at …

Due to the lack of observed groundwater table data and micro-scale topography of the
hillslopes constituting a watershed, quantification of subsurface flow using the existing …

Low streamflow statistic estimators at ungauged river sites generally have large errors and
uncertainties. This can be due to many reasons, including lack of data, complex hydrologic …

Hillslopes are a fundamental unit of surface hydrology, mediating the flow of water to fluvial
networks through overland flow and subsurface pathways. We present Arc Hydro tools to …

In this study, the time–area curve of an ellipse is analytically derived by considering flow
velocities within both channel and hillslope. The Clark IUH is also derived analytically by …

Yayılı kirletici kaynakların akarsudaki kirlilik yüküne etkisinin anlaşılabilmesi için, akım
bileşenlerinin doğru olarak belirlenmesi önemli bir ihtiyaçtır. Bu ihtiyaçtan yola çıkılarak …