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b. To impruve oc, maintain conulS 1; lake anci the <br />creek, over those which existed 1,rio, truction of the <br />Headwaters Control Structure. <br />SECTION III. UPEHATING IJIWC!_:UUHE: <br />The Headwaters Control Structure Is operated in accordance <br />with this section to accomplish thn Manage:,iient Goals in SECTION II. <br />The operating procedure requires discharges to occur within <br />the limitations of established discharge zo,ies described as <br />function of the Lake Minnetonka level. The ranges of discharise <br />defined by the -e zones are necessary rea1l:::n6 the numerous <br />considerations which must be t,iL.en into ac :ount during operation <br />of the structure. The discharge zones are based upon sound <br />hydrologic principles and are designed to achieve, to the `*eeatest <br />extent possible, the Management Goals iientified in SECTION I1. <br />"'he atta ched exhibit shows the di :ct ,,rt a zones and .heir <br />corr_,poridliL6 allowable: discharge rate. The lowest heavy line <br />across the base of the graph at elevati-n 928.6 represents the <br />minimum lake level elevation at watch discharge can occur. This <br />Is similar to the effect of t:,e previous fixed weir which had an <br />approximate low point elevation of 928.6. When the lake level is <br />above this elevation, a discharge will occur subject to the <br />conditions outlined in this section. The discharge zones are <br />defined by minimum required and/or maximum allowable discharge <br />rates over a specific time period and lake level ranee. These <br />zones are described in SECTIO14 III.A below. <br />Between lake level ele,,gtions 928.6 and 930.0 discharge to <br />Minnehaha Creek will vary. In general, discharge rites wall <br />increa-e as the lake level. increases. However, this Is not a <br />direct or linear relationship. The discharge is dependent not <br />only upon lake level elevation, but the time o: year, climatic <br />conditions, the variable carrying capac'_ty of the crt.:k and other <br />cons ide rat ions . <br />The heavy horizontal line at elevation 930.0 represents a <br />lake level above which high eater will be re('-;^.ed to the maximum, <br />practicable extent. Lame levels and dischart,- .snot be <br />controlled by the structure at lake level elevat ..,s above 930.0. <br />Unuer :.hese circumstances, resulting discharge to Minnehaha Creek <br />Is comparable to that whict, occurred under similar conditions with <br />the previous fixed weir. <br />Uuring the winter nt)nth which are not sh%wn on the attached <br />exhibit, no a-LounarL,e is all d to the extent 1'easible and <br />cons istant with the MANAGEMENT POLICY. Stop lobs are: Installed <br />during the late fall, prior to ice -in when the lake level <br />elevation is near 928.6. The discharge control gates are then <br />lifted out of the water to prevent ice damage. If the lake level <br />rises after that time, additional stop lugs are installed as <br />_j of 1 t <br />