Snowmelt is a major source of groundwater recharge in cold regions. Throughout many
landscapes snowmelt occurs when the ground is still frozen; thus frozen soil processes play …

Snowpack accumulation and depletion are important elements of the hydrological cycle in
the Canadian prairies. The surface runoff generated during snowmelt is transformed into …

This study evaluates the applicability of the chloride mass balance (CMB) method for
groundwater recharge estimation in a semi-arid region in Canada, where recharge largely …

In the cold semiarid Canadian prairies, groundwater recharge is focussed under numerous
topographic depressions, in which snowmelt runoff converges. Agricultural land uses on the …

Climate induced changes in runoff regimes and ongoing anthropogenic modification of land
use and land cover (LULC) are shifting ambient water quality signals worldwide. Modulation …

The role of hummocky terrain in governing runoff routing and focussing groundwater
recharge in the Northern Prairies of North America is widely recognised. However, most …

Snowpack accumulation and depletion are important elements of the hydrological cycle in
the prairies. The surface runoff generated during snowmelt is transformed into streamflow or …

The infiltrability of frozen soils strongly influences the partitioning of snowmelt and
hydrological functioning of cold regions. Preferential flow in macropores may enhance …

Numerical modeling of groundwater flow is a powerful tool that can assist in hydrogeological
analysis and understanding of groundwater system behavior. However, its results are highly …

Numerical groundwater modeling is an effective tool that provides insights into an aquifer
system behavior and can be used for groundwater management decisions. To produce …