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Modelling snow dynamics and groundwater-surface water interactions in mountainous, foothill and plain regions in North Saskatchewan River Basin, Canada
DownloadFall 2020
Snowmelt and groundwater-surface water (GW-SW) interactions are dominant controllers of hydrological cycles and water availability in northern latitudes that are characterized with ‘cold region hydrology’. Snowmelt is the main source of groundwater recharge and surface runoff, as snow...
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