Subarctic wetlands span almost one-sixth of the Canadian wetlands and have been acknowledged as an important ecotone between arctic tundra and boreal forest. Their hydrological complexity is determined by the climatological and physiographical characteristics with regard to the spatiotemporal distribution of water resources. In this study, two semi-distributed hydrological models, SLURP (semi-distributed land use-based runoff processes) and WATFLOOD TM , were employed to understand their effectiveness in modeling the hydrology of subarctic wetlands. Comparisons of their delineation approaches, formulations, parameters, and simulation results indicated that both models were capable of simulating the hydrological processes. However, differences were also observed. Besides their different segment delineation approaches, snowmelt and spring peak flows simulated by SLURP were 4-7 days earlier than those estimated by WATFLOOD because SLURP predefines snowmelt rates as variables, whereas WATFLOOD applies constants in the degree-day method. Due to the lack of considering the existence of permafrost and numerous seasonal ponds, both models tended to underestimate the spring peak flows. Evapotranspiration estimated by the Morton complementary relationship areal evapotranspiration method adopted in SLURP was lower than that calculated by WATFLOOD. Summer runoff only appeared during intense rainfall events, and its concentration was much faster in both models as compared with the observed records, which may be attributed to the variations of permafrost depth, soil water storage capacity, and seasonal pond levels. These findings will be helpful in improving the modeling quality of the two models and understanding the hydrologic features of subarctic wetlands.