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'''Baseflow''' (also called '''drought flow''', '''groundwater recession flow''', '''low flow''', '''low-water flow''', '''low-water discharge''' and '''sustained''' or '''fair-weather runoff''') is the portion of [[streamflow]] that comes from "the sum of deep subsurface flow and delayed shallow subsurface flow". It should not be confused with [[groundwater flow]]. [[Fair weather flow]] is called as [[Base flow]]{{dn|date=January 2017}}. <ref>{{cite journal |author=Kendall and McDonnell
|year= 1998
|title= Isotope Tracers in Catchment Hydrology