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Memo: Seneca II AHR - 2 - April 8, 1986 <br />Group 1 SW-S2-5 Group 2 NPDES 004 <br />SW-S2-1 SW-S2-6 <br />NPDES 002 <br />NPDES 003 <br />SW-S2-2 <br />The stations are grouped by receiving stream for maximum information barring <br />any unforeseen problems during sampling. Time constraints would probably <br />preclude monitoring both groups within a single day. <br />3. With the reduction to a tri-annual monitoring program, is the sampling <br />schedule for full-list analysis determined by time (seasonal) or flow <br />conditions? <br />If a mean annual representation is desired, sampling at intervals throughout <br />the year based on seasonal differences would be preferred. If monitoring is <br />to determine extremes of water quality, then a flow-dependent sampling is <br />required. This could be further defined into: 1. Low flow, cold <br />temperature; 2. High flow, cold or warm temperature; and, 3. Low flow, warm <br />temperature, when only three samples are allowed on an annual basis. <br />Condition No. 2 could be either a snowmelt event or a storm runoff event. I <br />was unable to determine from available correspondence which objective was <br />defined for monitoring under the reduced program. My preference would be to <br />sample based on extremes of flow. A clarification on this and a statement at <br />the beginning of discussion in Section V would be appreciated. <br />4. 'Stage-rating curves were included in the report as in 1984. The use <br />and purpose of these is uncertain. The gages constructed at surface sites are <br />of the crest-stage type which implies they are used for estimating unmonitored <br />data alone. Is this correct? <br />The ratings are said to be based on Manning equation velocities, of which no <br />indication of Manning "n" value is supplied in the report, or if different n <br />estimates are used as channel conditions change between high and low flows. <br />As Manning's n cannot be directly measured, then its use can give only a very <br />approximate estimate of flow for rating a station. <br />A more valid procedure for developing a stage-rating curve, if needed, would <br />employ a step-backwater analysis. Without going to this extent, however, the <br />existing curves could be improved by obtaining more calibration points at high <br />and low flows, periodic updating of the curve with recent observations, and/or <br />adjusting the best fit line into a curve at the lower end. If a considerable <br />improvement in station flow monitoring is desired, then construction of a weir <br />or other control along with continuous recorder is advised to improve <br />discharge monitoring. In future AHR's, the rating curves should be relocated <br />to Appendix D or omitted rather than included in the discussion section of the <br />report. <br />5. The daily flow tables could be improved by also calculating an annual <br />mean flow (in cfs) and an annual summation of flow volume (in acre-feet). <br />This would supplement reporting of flow conditions year-to-year in <br />quantitative terms and assist in the narrative discussion in the AHR. <br />