Evaluating the relative importance of shallow subsurface flow in a prairie landscape

Hydrologic literature on the Northern Great Plains, including the Canadian Prairies, has mainly focused on Hortonian overland flow as the dominant runoff generation mechanism. This study focused on subsurface water movement and its contribution to streamflow in high-latitude, subhumid, prairie lands...

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Veröffentlicht in:	Vadose zone journal 2017-05, Vol.16 (5), p.1-20
Hauptverfasser:	Ross, Cody A, Ali, Genevieve, Bansah, Samuel, Laing, Janelle R
Format:	Artikel
Sprache:	eng
Schlagworte:	antecedent wetness atmospheric precipitation Banks (topography) Canada Canadian Prairies Catfish Creek watershed drainage basins dye tracers Dyes feedback Flood peak fluid flow Freshwater Grasslands Great Plains ground water Groundwater flow Groundwater table Hydrogeology hydrologic cycle Hydrology isotope ratios isotopes Landscape levels Manitoba Moisture content North America Northern Great Plains O-18/O-16 Overland flow oxygen Plains porosity Prairies Rain Rainfall riparian environment Rivers Runoff Saturated soils Saturation seasonal variations shallow depth Slope Snow Snow cover Snow-water equivalent Snowmelt Soil Soil water southeastern Manitoba stable isotopes statistical analysis stormwater Stream discharge Stream flow Streams subsurface flow Subsurface water Surface runoff Topography Topography (geology) Tracers Transmissivity unsaturated zone Water Water table Western Canada
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