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- Q30036 subject Q6529368.
- Q30036 subject Q7029170.
- Q30036 abstract "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.Certain parameters of baseflow, such as the 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. 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 tracing and the software program HYSEP, among others.".
- Q30036 wikiPageExternalLink HYSEP.
- Q30036 wikiPageWikiLink Q13416553.
- Q30036 wikiPageWikiLink Q1444790.
- Q30036 wikiPageWikiLink Q2478921.
- Q30036 wikiPageWikiLink Q320062.
- Q30036 wikiPageWikiLink Q3983324.
- Q30036 wikiPageWikiLink Q4866642.
- Q30036 wikiPageWikiLink Q5611028.
- Q30036 wikiPageWikiLink Q6529368.
- Q30036 wikiPageWikiLink Q7029170.
- Q30036 comment "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".".
- Q30036 label "Baseflow".