Catchment hydrology of a High Arctic lake

摘要: Abstract In small lake catchments of the High Arctic, hydrologic processes are highly variable both spatially and temporally, so that single site measurements phenomena seldom representative catchment averages. Throughout spring summer, snow ice melts often occur alongside evaporation runoff from bare ground. The evaluation various quantities therefore is prerequisite upon an incorporation changing spatial patterns major processes. Through budgeting water inputs losses a typical its catchment, this study demonstrates dependence Arctic lakes their for supplies. turn, modify storage thus alter outflow regime catchments.