Large‐scale groundwater models are required to estimate groundwater availability and to
inform water management strategies on the national scale. However, parameterization of …

How topography controls topography‐driven groundwater flow is investigated with varying
rainfall and topography using a two‐dimensional groundwater‐surface water coupled …

Salinization is one of the main causes of conversion between different ecosystems and
landuse functions in coastal wetlands. In this paper, we studied the spatiotemporal dynamics …

This paper introduces a method of groundwater pollution source identification obtained from
laboratory by a physical instrument of Flow System Sand-Box Model. A Unit basin of a …

Groundwater mounds and depressions induced by rainfall and evapotranspiration near
wetlands/lakes have been widely observed, but their effects on groundwater flow field are …

Abstract Study region Central Pannonian Basin, Hungary. Study focus Critical Zone (CZ)
Science generally focuses on the soil and weathered bedrock in a few or tens of meters …

Groundwater–surface water interaction is greatly affected by surface topography and
agricultural activities in managed agricultural regions. Such an interaction increases the …

Hyporheic flow, which occurs in the shallow zone where river flow interacts with
groundwater (GW) flow, involves spatiotemporally complex water mixing and storage …

Study region Kamikochi area in the Japanese Northern Alps Study focus For mountains with
high precipitation and hydraulic gradients, understanding the hydrologic cycle is important …

Abstract Stampriet Transboundary Aquifer System (STAS) is shared between Botswana,
Namibia and South Africa with massive utilization especially in Namibia. However, the …