River-wetland corridors form where a high degree of connectivity between the surface
(rheic) and subsurface (hyporheic) components of streamflow creates an interconnected …

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

Recent developments in mascon (mass concentration) solutions for GRACE (Gravity
Recovery and Climate Experiment) satellite data have significantly increased the spatial …

A method for assessing the environmental impacts of freshwater consumption was
developed. This method considers damages to three areas of protection: human health …

Since tectonic subsidence in sedimentary basins provides the potential for long-term facies
preservation into the sedimentary record, analysis of geomorphic elements in modern …

Abstract The Okavango Panhandle is the main influent watercourse of the Okavango Delta,
an inland sink of the entire sediment load of the Cubango-Okavango River Basin (CORB) …

In arid central Australia, the∼ 1.14 Mkm2 endorheic Lake Eyre Basin (LEB) experiences
sporadic floods, and contains saline shallow groundwater. In this basin, where on-ground …

Hydrological and hydrodynamic models are core tools for simulation of large basins and
complex river systems associated to wetlands. Recent studies have pointed towards the …

Dams, diversion of water, invasive species, overharvesting and pollution are degrading
rivers and wetlands. Climate change may exacerbate impacts of these threats through …

Accurate inundation maps for flooded wetlands and rivers are a critical resource for their
management and conservation. In this paper, we automate a method (thresholding of the …