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The proposed West Vadnais outlet project involves water flow between three water <br />management organizations: Vadnais Lake Area WMO, Grass Lake WMO, and Ramsey - <br />Washington Metro Watershed District. Grass Lake and West Vadnais Lake may <br />exchange water during high water periods. Grass Lake elevation has been markedly <br />elevated since 2001 (extended periods above 882.7, 1988 datum), most obviously <br />encroaching on the I -694 Right -of -Way fence and flooding the bike pathway under <br />Gramsie Road in Shoreview. The highest point controlling flow between Grass Lake and <br />West Vadnais Lake is thought to be a culvert under a Metropolitan Council interceptor <br />sewer access road on the east side of Grass Lake, with bottom -of -pipe elevation of about <br />881.2 +/- (1988 datum, extrapolated from Profile 4, Grass Lake WMO Level Control <br />Plan, April, 1990). <br />Grass Lake's watershed is approximately 1,389 acres and includes outflow from Bennett, <br />Wabasso, Owasso and Snail Lakes in Roseville and Shoreview. Grass Lake is a shallow <br />lake, which has been largely vegetated until recent high -water conditions created a much <br />larger open -water area. The Grass Lake WMO Water Management Plan discusses the <br />important role of infiltration or seepage from Grass Lake into the groundwater. <br />Evapotranspiration by plants is also an important process, which consumes water in <br />Grass Lake during periods when vegetation is abundant in the .lake. According to long - <br />term.lake elevation data collected by Ramsey County, Grass :Lake is well below the high <br />point elevation connecting it to West Vadnais Lake (881.2 + / -, 1988 datum) for the vast <br />majority of time. An extended wet period (precipitation exceeding the annual average) <br />may reduce the rate of infiltration from Grass Lake and result in an increase in lake level. <br />It is at such tiriies that the Grass Lake elevation may be high enough to' move water. to <br />West Vadnais Lake. <br />The immediate watershed to West Vadnais Lake is small and water level in the lake <br />corresponds to local ground water levels and the water flowing into it from Grass Lake <br />on an •intermittent basis. The water levels of Grass Lake and West Vadnais Lake are <br />thought to be similar during high water periods, although there are limited West Vadnais <br />Lake elevation data to verify this belief. The proposed West Vadnais Lake outlet will <br />provide an outlet for both Grass Lake and West Vadnais Lake, on an infrequent basis, <br />into the Ramsey Washington Metro Watershed District and Gervais Lake. <br />Prior to construction of I -694, West Vadnais Lake's outlet was provided by surface flow <br />to the south, through Black Tern Lake and into Gervais Creek, flowing to Gervais Lake. <br />This flow path was eliminated by construction of the highway in the 1960's. A <br />secondary potential outlet from West Vadnais was then constructed incorporating a short <br />section of pipe and ditch (actually a deep ravine) to Twin Lake. Over time, the ravine <br />was filled in with demolition rubble and the east end of the pipe section was blocked and <br />eventually covered by a storm shelter building. The proposed West Vadnais outlet pipe <br />alignment ends at Jiggs Pond rather than Black Tem Lake because the water level of <br />Black Tern Lake has been manipulated (raised) over the years by development grading <br />and construction of an outlet pipe. <br />- 1 4 - <br />