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River flow, also termed discharge, is the volume of water moving past a point. Flow is measured in cubic feet per second (cfs) or cubic meters per second (cumecs). A hydrograph is a plot of flow over time.
River flow varies over time and space. Floods and low-flows occur, sometimes in a predictable seasonal pattern, and sometimes less predictably. Rivers in variable climates tend to have variable flows, while rivers that are dominated by groundwater tend to have very constant flows
“Flow regime” describes the pattern of flow variability for a particular river or region. Flow acts as a master variable, influencing the ecological integrity of river ecosystems. The natural flow regime: a paradigm for river conservation and restoration (Poff et al. 1997) describes the many biological consequences of altered flow regimes. |
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| “The ecological integrity of river ecosystems depends upon their natural dynamic character” (Poff et al. 1997) | ||||
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Signing up for the Natural Flow Regime listserve
This listserve will connect on-the-ground practitioners, university scientists, agency personnel, non-governmental organizations, planners, and local officials working on natural flow regime restoration and management in the Great Lakes basin. The intent is to provide an easy-to-use vehicle to promote communication and coordination among groups that are testing the flow regime paradigm as a master variable for ecological restoration. To sign up for the Natural Flow Regime listserve:
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