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2018-03-12-minutes-public-works-study-session
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2018-03-12-minutes-public-works-study-session
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5/12/2020 2:00:27 PM
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Meeting
Date
3/20/2018
Meeting title
Commissioners' Agenda
Location
Commissioners' Auditorium
Address
205 West 5th Room 109 - Ellensburg
Meeting type
Regular
Meeting document type
Supporting documentation
Supplemental fields
Alpha Order
a
Item
Approve Minutes
Order
1
Placement
Consent Agenda
Row ID
43308
Type
Minutes
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occurs in the Unnamed Tributary 8 model (Figure 8). There is a large gap in the cross <br />sections and therefore a large gap in the floodplain delineation. <br />9. Disconnected Floodplain Areas — Pools of water disconnected from the main channel <br />show up in many of the modeled Zone A floodplain delineations. Automated mapping <br />procedures for HEC -RAS often produce such disconnected areas, but these are typically <br />either removed in final mapping or physically connected to the main channel delineation. <br />WSE assumes these problems will be corrected in the final mapping. <br />Zone AE Detailed Study of the Yakima River from Easton to Cie Elum <br />In general, the Zone AE model for the Yakima River from Easton to Cie Elum appears <br />reasonably wall developed; however, Issues have been identified which are described below <br />and presented in Figure 9. <br />Hydrology — STARR has reduced the magnitude of the 100 -year flow significantly which <br />is the primary reason BFEs in the new study are lower and floodplain inundation limits <br />are reduced when compared to the effective study. For example, the new model uses a <br />flow of 24,095 cfs at a location just downstream of the confluence with the Teanaway <br />River (cross section 85147), while the effective model uses 29,100 cfs at the same <br />location (FEMA, 1981). Similarly, just upstream from the confluence the new model <br />uses 19,828 cls while the effective model uses 25,200 cfs. Documentation as to how <br />the new discharge was computed was not provided. WSE would like to review the <br />hydrology calculations developed for this study. <br />2. Cross Section Orientation and Data — Several cross sections appear to be skewed <br />significantly to the direction of flow or contain data errors. Several examples are <br />highlighted in Figure 9. <br />3. Definition of Ineffective Areas -- Ineffective flow areas are defined liberally throughout <br />the Yakima River made[, and most appear logical. However, WSE noticed a number of <br />instances where continuity of flow along a floodplain is interrupted by questionable <br />Ineffective flow designations. WSE recommends that STARR conduct a simple review <br />of all ineffective areas to double check for continuity of down valley flow. <br />In several reaches the 500 -year flood is conveyed through the floodplain at one cross <br />section, but not the next. It appears Ineffective elevations were set to accommodate the <br />100 -year event, but not the 500 -year. Ineffective elevations need to be adjusted or <br />ineffective areas added or deleted such that flow remains either consistently effective or <br />Ineffective along a reach during the 500 -year flood; unless features are present that <br />physically do block flow. <br />4. Downstream Boundary Condition - Normal depth procedures are used to estimate the <br />downstream boundary condition for each profile; however, the slope applied appears to <br />be too flat when compared to the slope of the river, valley, and energy grade line. <br />4 <br />
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