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Overview of Index Ratings Process. Streamflow Records Computation using ADVMs and Index-Velocity Methods Office of Surface Water. Goals for this Presentation. Index-velocity Method. Channel area is computed at a specific, selected location using a stage-area rating
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Overview of Index Ratings Process Streamflow Records Computation using ADVMs and Index-Velocity Methods Office of Surface Water
Index-velocity Method • Channel area is computed at a specific, selected location using a stage-area rating • Mean-channel velocity is computed from the index velocity measured by an instrument using an index-to-mean velocity rating
Stage and Area • Flow area changes with stage • A stage-area rating must be developed for a selected “standard” cross-section to compute flow area for a range of stages • Standard cross section should be surveyed • Stage-area rating is developed from survey data
Standard Cross Section • Q1 = Q2 = Q3 • Area is always computed at location 1! 1 2 3 1 = standard cross-section 2 = wading measurement section 3 = bridge measurement section
Index Ratings • ADVMs measure a portion of the channel (Vi); mean channel velocity is not measured • Thus we need to relate the index velocity,Vi,(ADVM measured velocity) to the measured-mean channel velocity (from discharge measurements)
Simple Linear Rating Example Rating Example Rating
Compound Linear Ratings Plot data Hydraulic basis for compound rating? A Vm B Example Rating Vi
Compound Linear Ratings High end Low end Final Rating w/ Transitions
Multiple Linear Ratings Data plots Residual plots Change in flow distribution with stage? Significant variation in stage?
Multiple Linear Ratings Residual plots Vm = 0.82*Vi – 0.15(Stage*Vi) + 0.16
Computing Continuous Discharge • For every stage, an area (A) is computed from the stage-area rating • For every index velocity (Vi) a mean cross-sectional velocity (Vcomp) is computed from the index rating • For every time step, discharge is computed using the equation Q = Vcomp*A (unit values of Q) • The discharge record is published (e.g. mean daily flows or tidally-filtered flows)