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Routine Office Techniques. Streamflow Records Computation using ADVMs and Index-Velocity Methods Office of Surface Water. Overview. Real-time data. Daily data review. Check to see that: Index-velocity is in expected range Cell-end has not changed SNR is in expected range
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Routine Office Techniques Streamflow Records Computation using ADVMs and Index-Velocity Methods Office of Surface Water
Real-time data • Daily data review. Check to see that: • Index-velocity is in expected range • Cell-end has not changed • SNR is in expected range • ADVM temperature is reasonable • Cross-stream velocity has not unexpectedly changed
Cell End • Extreme example of a cell end that is not appropriate for the conditions in the field
Signal Amplitude • Unusually high variation in signal amplitude
Internal ADVM data review • Some parameters recorded internally cannot be transmitted • Velocity in beam coordinates • Multi-cell data 6-10 • Individual beam signal amplitudes/SNRs • Internal diagnostic beam check recorded at specified interval • Pitch, roll, heading (if available) • Pressure • Velocity standard error
XY Velocity – Typical Pattern Vel X Vel Y
Beam Velocity – Typical Pattern Beam 1 Beam 2
Beam Velocity – Atypical Pattern • Multi-cell velocity • BEAM COORDINATES • Beams are looking at different water conditions • Probably located in an eddy • Meter was moved 200 ft into the flow BEAM 1 BEAM 2
Multi-cell Data – Typical Pattern • Cells 1,3,5,7,9 shown here
Beam Amplitude/Instrument Noise Level • Individual signal amplitude plots can give more information then transmitted average SNR. For the example here, beam 1 probably had something blocking it for a small period of time, but the transmitted SNR would still have looked reasonable
Internal Diagnostics Cell begin Cell end
Pitch / Roll Pitch, roll and heading should not change more than 2 degrees over a deployment. In this example, the pitch is fine, but the roll should be watched to assure it does not drift more than shown here
Vertical Beam / Pressure • For sidelooking systems, pressure helps to determine a “gate” for the vertical beam depth. • The vertical beam can easily be fouled as sediment and debris settle onto the ADVM. Pressure CANNOT be used as a vertical beam substitute
Cell End / Water Depth • For uplookers, the cell end and water depth should match closely as the water depth helps determine where the cell ends when dynamic boundary is set up Argonaut-SW Argonaut-XR
Velocity Standard Error Beam 1 Beam 2 Cell 1 Cell 7Cell 9
Additional QA/QC • Temperature • Sensor failure can be obvious (a sudden jump to an unreasonable value) or can occur over time. • A temperature error of 5 C can result in a 1 to 1.3% bias in velocity • Currently, no easy way in NWIS to compare temperature record to environmental measurements stored in SiteVisit. Spreadsheet logs are still necessary
Additional QA/QC • Signal Amplitude / Instrument Noise Level • It is not necessary to look at SNR, signal amplitude, and instrument noise level, since SNR is computed from signal amplitude and instrument noise level. • Finding an unreasonable signal amplitude value in the field will indicate major problems. However, there could be a systematic change in the signal amplitude (steadily decreasing for instance) that can easily be missed in the field if the value is reasonable and you are not looking over a long period of time. • The instrument noise level should be examined for pattern changes as well
Miscellaneous Office Tasks • Archival • Index-velocity parameters within SiteVisit • Anything relating to rating development and maintenance is discussed elsewhere
SiteVisit • There are a couple of index-velocity specific fields and reports within SiteVisit • Under the discharge measurement section if the box next to “Index Velocity Site” is checked the following boxes will become available
SiteVisit • Mean Index Velocity – the average index velocity for the measurement • Standard Section Area – The area from the stage-area rating • Standard Section Velocity – Mean channel velocity – computed automatically if area is entered (Q in this example was 3,460 cfs)