'Low flow periods' presentation slideshows

Surface Water Hydrology

Surface Water Hydrology. Summarized in one equation. V = velocity, fps or m/s A = channel cross-sectional area, sf or m 2. A. V. Stream Discharge (Q). Fundamental stream variable Cubic feet/second (cfs, ft -3 sec -1 ) Q=V*A Velocity (ft/sec) * Channel area (ft 2 ) Instantaneous.

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River Monitoring and Climate Change Conference Leominster, MA May 18, 2011 Sponsored by

329 views • 22 slides