Subsurface permeability is a measure of how well liquids flow through below-ground rocks and soils. It is a key parameter that determines subsurface flow and transport processes in watersheds. However ...

River discharge and temperature are key indicators of change in hydrologic systems. Coupled daily streamflow and river temperature data provide extremely useful datasets in regions that otherwise ...

In the McMurdo Dry Valleys, Antarctica’s largest ice-free area, the stream channels consist of rock and soil that is underlain by permafrost. Substantial permafrost degradation and channel erosion ...