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The continuous slope-area method for computing event hydrographs

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The continuous slope-area method for computing event hydrographs; 2010; SIR; 2010-5241; Smith, Christopher F.; Cordova, Jeffrey T.; Wiele, Stephen M.

Summary

The continuous slope-area (CSA) method expands the slope-area method of computing peak discharge to a complete flow event. Continuously recording pressure transducers installed at three or more cross sections provide water-surface slopes and stage during an event that can be used with cross-section surveys and estimates of channel roughness to compute a continuous discharge hydrograph. The CSA method has been made feasible by the availability of low-cost recording pressure transducers that provide a continuous record of stage. The CSA method was implemented on the Babocomari River in Arizona in 2002 to monitor streamflow in the channel reach by installing eight pressure transducers in four cross sections within the reach. Continuous [...]

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Type Scheme Key
local-index unknown sir20105241
local-pk unknown 99106
doi http://www.loc.gov/standards/mods/mods-outline-3-5.html#identifier doi:10.3133/sir20105241
series unknown Scientific Investigations Report

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journalScientific Investigations Report
edition-
languageENGLISH
citationTypeReport

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