“…To help better understand and predict the water cycle, hydrological modelling has been playing a significant role in studying the distinguished attributes of subarctic wetlands. Numerous models have been developed and applied for hydrology simulation, such as hydrologic engineering center (HEC-1), semidistributed land use-based runoff process (SLURP), precipitation-runoff modelling system (PRMS), streamflow synthesis and reservoir regulation (SSARR), snowmelt runoff model (SRM), UBC, WATFLOOD, and TOPMODEL (Quick and Pipes, 1977;Beven et al, 1984;Abbott et al, 1986;Bergström, 1992;Kouwen et al, 1993;Bicknell et al, 1997;Kite, 1997;Richard and Gratton, 2001;Chen et al, 2003Chen et al, , 2004Chen et al, , 2007Chen et al, , 2008. However, only a few studies specifically targeted at subarctic wetlands, particularly the HBL in northern Manitoba due to a number of knowledge gaps, such as the difficulty of considering continuous permafrost, numerous seasonal ponds, and snow sublimation as well as the complexity of simulating water linkage between surface and subsurface flows in the hummocky terrain (Mancell et al, 2000;Zhang et al, 2000;Van der Linden and Woo, 2003;Boswell and Olyphant, 2007).…”