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{{Short description|Stream flow between precipitation events}}
'''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 the [[streamflow]] that is sustained between precipitation events, fed to streams by delayed pathways. It should not be confused with [[groundwater flow]]. Fair weather flow is also called base flow.<ref>{{cite journal
|author= Kendall and McDonnell
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