Laserfiche WebLink
<br />00 <br />c'() <br />--.j.t <br />C'J <br /> <br />'..~.J <br /> <br />C_' <br /> <br />the control .flow is 2000 e.f.s. Tho forecasting lUll! evacuating procedures <br /> <br />have already been developed and tested. At present, the forecasts are <br />based on a combination of snow survey records, precipitation records and <br />temperature records. Witll each passing year, the forecasts will be re- <br />e.,.."mintad to evaluate possible revisions or add1tiOIll9 in an effort to <br />reduce or e) im1 nAte errors. At presen1;, the III10il ~ records do not <br /> <br />extend over a very long period. It is prellllllled that the chances of error <br />will be materially reduced by increased lengths of record. <br />Inflow to Platoro Rese1wir is 1'rom rl1lllla.rOUS iImall creeks and <br />springs and also precipitation in the reservoir area. The amount of <br />inf'low will be d.etermined 1'rom records of releases, ~""glO in storage 8IIIl <br />evaporation. A gaging station is to be installed immediately below Platol'O . <br /> <br />Dam to measure releases. <br /> <br />amount of reservoir water entering each ditch (reservoir water being c0n- <br />sidered as the release .from the reservoir minus the inflow to the reservo;lr <br />less the estimated transportation loss from Platoro to MogGte). <br /> <br /># <br />