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Certain parameters of baseflow, such as the [[mean baseflow residence time|mean residence time]] and the baseflow recession curve, can be useful in describing the mixing of waters (such as from precipitation and groundwater) and the level of groundwater contribution to streamflow in catchments. <ref>{{ cite journal
|author=Vitvar
|year=2002
|title= Estimation of baseflow residence times in watersheds from the runoff hydrograph recession: method and application in the Neversink watershed, Catskill Mountains, New York |url=http://www.cof.orst.edu/cof/fe/watershd/pdf/2002/Vitvar_et_al_2002.pdf
|journal=Hydrol. Processes
|volume=16
|pages= 1871–1877|display-authors=etal}}</ref>
[[Hydrograph separation|Baseflow separation]] is often used to determine what portion of a streamflow [[hydrograph]] occurs from baseflow, and what portion occurs from [[overland flow]]. Common methods include using [[isotope hydrology|isotope tracing]] and the software program [http://water.usgs.gov/software/HYSEP/ HYSEP], among others.
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